Sunday 18 September 2011

Department of Chemical Engineering at BUITEMS


Department of Chemical Engineering


Establishment of Chemical Engineering Department at BUITEMS was an urgent need of
Balochistan province, which needs industrialization at an accelerated pace. This is based on
the fact that this province is full of minerals, oil and gas resources.
One of the main attractions of Balochistan is its unexploited geological potentials. It occupies a
strategic location in relation to central Asia and sits on geological belts with known world-class
mineral deposits. Balochistan produces 40.2 % of the primary energy of Pakistan in the form of
natural gas, coal and electricity, of the total mineral fuel reserves of the country, Balochistan
contains more than 33 % of the natural gas, about 9% of the coal and about 2% of the probable
oil reserves.
A little has been done uptil now for the exploitation of these rich resources. This needs chemical
/metallurgical industries for the processing of valuable minerals and for the manufacture of
petrochemical products from the available oil and gas deposits in this province.

SCOPE

o There are a lot of opportunities for Chemical engineers in Pakistan
and abroad, as they deal with applying scientific and mathematical
principles, synthesizing new materials, transforming combinations of
elements of matter and developing the processes to do it all safely,
efficiently and on a large scale.
o Chemical engineers turn raw materials into valuable products. They
will often specialize in a particular area once they become established,
including biochemistry, the environment or petrochemical refining.
o Chemical engineering largely involves the design and maintenance of
chemical processes for large-scale manufacture.

VISION

o To be the leading Chemical Engineering department in Pakistan with
innovative and improved programs.
o To be the prolific department in providing the highly trained graduates
needed in the chemical and petrochemical production facilities
located in Pakistan and the Gulf Coast area.
o To achieve national and international recognition through the
educational and research achievements and the professional
service of our faculty, staff and students.

MISSION

The Department of Chemical Engineering is committed to establish conductive
environment for top class professional education and research in the field of
Chemical Engineering. The Department is committed to produce quality Chemical
engineers with expertise in operation and design of Chemical processes and their
modifications.
The Department of Chemical Engineering is also devoted to solve the industry's
technical and managerial issues targeting not only the current needs of industry but
also acting as a key source of ideas and expertise for the long term competitiveness
of the entire Chemical industry of Pakistan. This will also be source centre for
technical human resources, executives and consultants.

OBJECTIVES

o To produce professional Chemical Engineers (men and women) of
high calibre and expertise to meet the demand of Chemical /
Petrochemical industry of Pakistan.
o After graduation, Chemical Engineers of this University will serve in
Oil & Gas industry, SANDAK Project. Sui (PPL), Pirkoh, Loti, Uch,
Zin, Jandran of OGDCL & BG, BOSICOR refinery, HUBCO Pvt. Ltd.,
provides another prospect of utilizing their skills as a Chemical
Engineer.

o To enable the youngsters of Pakistan in general and youngster of
Balochistan in particular to acquire expertise in the different areas/fields
of Chemical Engineering.
o To develop trained human resources for Chemical process industry of
Pakistan.
o To analyze industrial Chemical Engineering Problems and synthesize
solutions to those problems, compare favourably in their knowledge of
chemical engineering.
o To use their training as a springboard to further professional and
career development.

Department of textile engieering at BUITEMS


Department of Textile Engineering

Introduction

Balochistan having fertile land and growth environment is quite suitable for growing cotton.
Balochistan is also rich in wool production. Keeping in view the need of expertise in the field
of wool processing in particular and cotton / manmade fabrics in general, BUITEMS launched
the BS Textile Engineering program with the intake of 20 students in Fall 2004 at Takatu
Campus in the former Bolan Textile Mills, Baleli, Quetta with the high spirit and hope to produce
quality textile engineers with the expertise in processing the wool, cotton and manmade fabrics.
It is an accredited program by the Pakistan Engineering Council.
After graduation, Textile Engineers of this University will serve in the textile industry of
Pakistan particularly the areas of Hub district Labella which caters more than 30 textile units. In
near futur Gawadar will be the Centre of industrial zone and demand of Textile Engineers will be
increased.

VISION

o BUITEMS should be one of the best in producing quality textile
engineers for the textile industry.
o To Make the department a Centre of Excellence in education and
research on textiles including operation and design of textile
processes and machinery.
o To Solve the industry’s technical and managerial issues.
o To become a major source of ideas and expertise for the long term
competitiveness of the entire textile industry of Pakistan.

MISSION

The Department of Textile Engineering believes in establishing conducive
environment for top of the class professional education and research in the field of
Textile Engineering. The Department is committed to produce quality textile
engineers with expertise in operation and design of textile processes and machinery.
The Department of Textile Engineering is also devoted to solve the industry’s
technical and managerial issues targeting not only the current needs of industry but
also acting as a key source of ideas and expertise for the long term competitiveness
of the entire textile industry of Pakistan. This will also be source centre for technical
human resources, executives and consultants.

OBJECTIVES

o To produce professional textile engineers of high calibre and expertise
to meet the demand of textile industry of Pakistan.
o To enable the youngsters of Pakistan in general and youngster of
Balochistan in particular to acquire expertise in the different areas /
fields of textile engineering.
o To develop trained human resources for textile process industry and
textile machine manufacturing industry of Pakistan.
o To establish a Centre of Excellence in textile engineering in general
and wool development and processing in particular.

OUTCOME OF THE DEPARTMENT

The Department intends to produce 40 to 50 BS Textile Engineering, 10 to 20 Master’s
in Textile Engineering and 1 to 5 PhD in the near future. Present intake is from 35-50
students each year.
The courses offered by the Department of Textile Engineering are intended to result
in:
o Minimization of unemployment.
o Improvement of living standard of the people of Balochistan
o Industrialization in the province
o Improvement of technical and scientific approach for production of
textile commodities.
o Effective utilization of textile resources of the province (wool/ cotton)
o Inducement of entrepreneurship (textile industry), in Balochistan as
well as Pakistan.

Department of petroleum and gas at BUITEMS


Department of Petroleum & Gas Engineering


Introduction

Balochistan is rich in natural resources like Oil, Gas and Minerals. The largest
reserves of gas exist in the area of Sui of this Province, which meets one-third of the country’s
energy requirements. Therefore keeping in view this essential need a department of Petroleum
and Gas was initiated in the fall of 2004 as the first and pioneering department in the then newly
established Faculty of Engineering and Applied Sciences (later renamed as the Faculty of
Engineering since September 2007.




SCOPE




o Pakistan’s current daily oil & gas production have reached 70,000
barrels of oil and 4 Billion cubic feet of gas repectively.
o Presently, 42 companies are working in Pakistan which have been
awarded 118 exploration licenses and 127 leases.
o Seventeen new blocks have been opened which would support the
ongoing exploration activities in the country and open major
opportunities for the prospective investors in diversified fields.
o Department of Petroleum and Gas Engineering program imparts to its
students modern scientific and computer skills for exploration,
development and exploitation of the oil and gas reserves and to
apprise them of the technological advances in Drilling, Production and
Reservoir Engineering as well as Safety with special reference to
Environments.
o Petroleum engineers produced by the department will be absorbed in
exploration & production, plus service and marketing activities of
national and multinational Companies of the world.

VISION


o BUITEMSshould be one of the best institution in the country to produce
quality petroleum engineers for the petroleum industry.
o To make the department a Centre of Excellence in education and
research on petroleum including reservoir, production and drilling
techniques for oil and gas fields.
o To solve the industry's technical and logical issues by using advanced
software and calculations.
o To become a major key source of ideas and expertise for the long term
competitiveness of the entire petroleum industry of Pakistan.

MISSION


The Department of Petroleum & Gas Engineering is committed to use
modern institutional technology to enhance learning and continue a
program of excellence in research to provide students with the necessary
skills to achieve success in their future professional careers not only in
Pakistan but also in the rest of the world.

OBJECTIVES


o To enable graduates to understand the importance of professional
responsibility and high ethical standards.
o To Produce engineers to assume positions of technical leadership in
the industry making use of their specialized knowledge of petroleum
engineering.
o To promote effective oral and written technical communication skills to
meet the challenges of the future petroleum engineering profession.
o To provide students with an education back ground in the
fundamentals, enabling them to succeed in graduate studies and
research in petroleum engineering.

OUTCOME OF THE DEPARTMENT


The Department of Petroleum & Gas Engineering intends to produce 40-50 Petroleum
Engineers with BS degree in Petroleum & Gas Engineering each year.
The Department intends to produce 10-20 MS degree holders and 1-5 Ph.D degree
holders in Petroleum and Gas Engineering.
The Department has already produced up to 100 Petroleum Engineers with BS
degrees from three (3) Batches.
o The courses offered by the Department of Petroleum & Gas
Engineering are intended to result in:
o Minimization of unemployment.
o Improvement of living standard of the people of Balochistan.
o Industrialization in the province.
o Improvement of technical and scientific approach for production of Oil &
Gas.
o Effective utilization of oil & gas resources of the province.
o Inducement of entrepreneurship (Petroleum & Gas Industry in
Balochistan and as well as in Pakistan)

Computer Networks complete notes

Geologic Resources complete notes


Mineral Resources

Building

Stone, Sand, Gravel, Limestone

Non-metallic Minerals

Sulfur, Gypsum, Coal, Barite, Salt, Clay, Feldspar, Gem Minerals, Abrasives, Borax, Lime, Magnesia, Potash, Phosphates, Silica, Fluorite, Asbestos, Mica

Metallic Minerals

  • Ferrous: Iron and Steel, Cobalt, Nickel
  • Non-ferrous: Copper, Zinc, Tin, Lead, Aluminum, Titanium, Manganese, Magnesium, Mercury, Vanadium, Molybdenum, Tungsten, Silver, Gold, Platinum

Energy Resources

  • Fossil Fuels: Coal, Oil, Natural Gas
  • Uranium
  • Geothermal Energy

Types of Ore Deposits

  • Magmatic: Pt, Cr, Fe, Ni, Ti, Diamond
  • Pegmatite: Li, Be, U, Rare Earths, Feldspar, Mica, Gems
  • Hydrothermal:
    • 600 C: W, Sn
    • 400 C: Au, U, Ag, Co, Mo
    • 200 C: Cu, Zn, Cd, Pb
    • Cool: Hg, As
  • Sedimentary Rocks: Fe, Cu, U, Mn, Mg
  • Weathering:
    • Secondary Enrichment: Cu, Ni
    • Soils, Al, Ni
  • Placer: Pt, Au, Sn, Ti, W, Th, Rare Earths U (Fossil), Gems

Concentration Factors and Economics

  • Natural Abundance
  • Geologic Processes to Concentrate Element
  • Intrinsic Value of Material
  • Cost of Extraction from Earth

Prospecting and Exploration

  • Satellite and Aerial Photography
  • Remote Sensing
  • Geological Mapping
  • Geochemical Sampling
  • Magnetic Mapping
  • Gravity Mapping
  • Electrical Sounding
  • Radioactivity Mapping
  • Seismic Methods
  • Reflection - Detailed but Expensive
  • Refraction - Cheap but Not Detailed
  • Core Sampling and Well Logging

Mining

  • Surface: Strip, Open-pit
  • Placer: Dense Minerals in Alluvium Underground

Economic Factors in Mining

  • Richness of Ore
  • Quantity of Ore
  • Cost of Initial Development
  • Equipment, Excavation, Purchase of Rights
  • Operating Costs
  • Wages, Taxes, Maintenance, Utilities
  • Price of the Product
  • Will Price Go up or down?

Life Cycle of a Mine

  • Exploration
  • Development
  • Active Mining
  • Recovery of Ore
  • Crushing, Milling, Flotation, Chemical Separation
  • Smelting and Refining
  • Disposal of Waste (Tailings)
  • Shut-down

Issues in Mineral Exploitation

  • Who Owns (Or Should Own) Minerals?
    • Landowner, Discoverer, Government
    • Unclaimed Areas: Sea Floor, Antarctica
  • Who Controls Access for Exploration?
    Remote Sensing vs. Privacy
  • Hazards of Mining
    • Safety
    • Mine Wastes
    • Pollution
      • Dust
      • Sulfur (H2SO4)
      • Acid Rain
      • Acid Runoff
      • Dissolved Metals (Fe, Cu, Zn, As...)
    • Noise
    • Environmental Problems
      • Exploration
      • Construction and Operation
  • Economic Impact
  • "Boom and Bust" Cycles

Geothermal Energy: A Free Lunch?

Environmental Problems of Geothermal Energy

  • It is Finite
  • Heat Sources Can Be Exhausted (Geysers, California)
  • Sulfur Emissions
  • Disposal of Mineralized Brines

Technical Problems of Geothermal Energy

  • Corrosion
  • Mineral Deposition in Pipes
  • Non-Productive gases (Carbon dioxide, methane, etc. These do not condense like steam, hence reduce efficiency. Must be removed)
  • Low Temperatures
  • Low Thermodynamic Efficiency

Thermodynamic Efficiency

Thermodynamic Efficiency is defined by the Second Law of Thermodynamics. It is the maximum possible efficiency any heat-driven process could produce, before any practical considerations like friction, heat losses, etc. The formula for thermodynamic efficiency is:
Eff. = (Ti - Tf)/Ti
(T = Degrees Kelvin = Degrees C + 273)
(Ti = initial temperature, Tf = final temperature)

Automobile Engine

  • Ti = 1200 C = 1473 K
  • Tf = 500 C = 773 K (If you don't believe this, drive for a half hour or so and then touch your exhaust manifold!)
  • Eff = (1473 - 773)/1473 = 48%
One of the fondest popular fantasies is that there is a device being kept secret by the oil companies and car manufacturers that would allow cars to get hundreds of miles per gallon. As this calculation shows, no amount of tinkering with the engine will do much better than double gas mileage (actually much less). Most of our improvements in gas mileage have come from reducing weight, air resistance and friction. This is one reason why most new cars have spare tires about the size of bagels, for example.

Typical Steam Power Plant

  • Ti = 700 C = 973 K
  • Tf = 200 C = 473 K (This is what the big cooling towers at power plants are for - to drop that final temperature and maximize Tf-Ti.)
  • Eff = (973 - 473)/973 = 51%
Critics of current energy practices point out that most energy is used to produce temperatures below the boiling point of water, and ask if it makes sense to have power plants generating extremely high temperatures. The answer is yes; it results in high thermodynamic efficiency. Attempting to supply hot water or hot air directly would lose far more energy in transmission losses than it would save in heating bills.

Geothermal Power Plant

  • Ti = 150 C = 423 K
  • Tf = 80 C = 353
  • Eff = (423 - 353)/423 = 17%
This Is Before Any Engineering and Operating Losses. The situation above is actually a very favorable one as geothermal power sources go. Actual achieved efficiencies:
  • Automobile on Highway: about 5%
  • Geothermal Plant: 5% or So, Sometimes less than 1%

Who's Got the Oil?

According to one comprehensive listing of the world's great oil fields, the total known oil reserves (including amounts already extracted) total 2100 billion barrels. These are concentrated in:
  • 8 fields with more than 30 billion barrels; total 290 billion or 14%
  • 24 fields with 10-30 billion barrels; total 363 billion or 17%
  • 95 fields with 2-10 billion barrels; total 407 billion or 19%
  • 385 fields with 0.5-2 billion barrels; total 341 billion or 16%
  • 18,000 fields with less than 500 million barrels: 700 billion or 34%
The pattern is clear: oil is overwhelmingly concentrated in a small number of giant and supergiant fields. There are not many places left to hide something that big. The discovery rate of giant fields has been falling for decades.

Giant Oil Fields

oil field statistics
The figure above shows the proportion of the world's oil reserves in fields of various sizes.

oil field statistics
The figure above shows the regional location of oil fields larger than one billion barrels. Note the overwhelming importance of the Middle East. The two largest fields are Gharwar in Saudi Arabia and Burgan in Kuwait. Still wonder why we fought the Gulf War?

Is There a Lot More Undiscovered Oil?

  • 80 per cent of oil being produced today is from fields discovered before 1973.
  • In the 1990's oil discoveries averaged about seven billion barrels of oil a year, only one third of usage.
  • The discovery rate of multi-billion barrel fields has been declining since the 1940's, that of giant (500-million barrel) fields since the 1960's.
  • In 1938, fields with more than 10 million barrels made up 19% of all new discoveries, but by 1948 the proportion had dropped to only 3%. Most oil fields are less than ten million barrels, and ten million barrels will supply the United States with less than a day's worth of energy. Large oil fields make up a disproportionate part of the world's oil supply. The ten largest oil fields contain a fifth of the world's oil reserves; twenty more bring the total to a third. 500 large fields contain two thirds of the world's known oil. The remainder is distributed among 20,000 or more small oil fields. The fact that discoveries of large fields are getting rarer means only one thing: we are running out of new oil to find.

Is the Energy Crisis a Myth?

One of the clearest analyses of the energy crisis is Energy Sources -- The Wealth of the World, by Eugene Ayres and Charles A Scarlott, two industrial scientists. This work is worth quoting in some detail.
The internal-combustion engine used for automobiles is a fragile device compared with other prime movers -- even compared with the internal combustion engines used for diesel- electric locomotives that have been known to go over a million miles without mechanical overhauling.
Something about the possession and operation of a motor car provides effective anesthesia for any awareness of economy ... A few people for technical reasons keep an account of miles per gallon of fuel, depreciation per mile, and other costs of motoring, but the result is usually so appalling that the accounts are hurriedly discontinued and forgotten.
The advertising specialists, conscious of the public pulse, do not waste much space and money talking about economy. They talk instead, of performance, comfort, style and reliability. Nearly everything said about a new car means lower fuel efficiency ...
... the energy-system efficiency of the motor car with petroleum motor fuel is, thus, 5 percent ... no one is proud of this accomplishment -- least of all the automotive-design engineers ... The trouble is, every time the design engineer manages to save a few BTU it is more than spent answering the clamor for softer tires, for radio, for better heaters, more lights, cigarette lighters and possibly even air conditioning.
Histories written a few centuries hence may describe the United States as a nation of such extraordinary technologic virility that we succeeded in finding ways of dissipating our natural wealth far more rapidly than any other nation. At any rate, we are having a wonderful time doing it. From the discussions in the earlier chapters of this book it is clear that the problem of energy for the United States is not one of the dim future. It is upon us now.
You may wonder why this book was quoted at such length; after all, it is little different from what energy analysts say all the time, although some of the remarks are clearly dated. These quotes are pretty much the same as any contemporary energy study, with one very important difference. They were written in 1952! Here's how Ayres and Scarlott viewed our future oil supplies.
Our imports of petroleum are small but each year they become larger. By 1960 they are likely to be quite substantial. By 1970 they will almost certainly be huge -- if foreign oil is still available then in sufficient quantity (emphasis mine) ... This tiny period of earth's life, when we are consuming its stored riches, is nearly over ... Fortunately for us there is still time for fundamental research [on alternative energy sources]. But not too much time.
There it is, all laid out with clockwork precision almost fifty years ago. We cannot say we weren't warned or that we were taken by surprise.
The unmistakable signs to those who were willing to see go back even further in time. As noted earlier, even before World War II the number of discoveries of new large oil fields was declining.
The person who has done the most to develop resource prediction strategies is M. King Hubbert. Hubbert is no neglected prophet but a long-respected petroleum geologist. Hubbert noted that the production history of an oil field follows a bell-shaped curve; increasing development, a production peak, then decline as the field is depleted. The cumulative production curve, which is actually a graph of the area under the bell curve with time, is a gentle S called the sigmoid curve. Oil fields often consist of a number of disconnected reservoirs, so if the curve applies to a single field it might also apply to a region, a state, a nation, or even the entire world. Hubbert also noted that production from new oil fields typically lags behind discovery by about ten years. In 1958, Hubbert noted that new discoveries in the U.S. had already peaked and were declining, and he predicted that U.S. oil production would peak in the late 1960's; it peaked in 1967. There was a later surge after the North Slope oil fields were discovered, but based on what was known in 1958, Hubbert was right on target.
Hubbert's curve has an interesting property. The sides of the bell-shaped curve rise steeply, and most of the area, or total production, is in a narrow band under the peak. Because of this geometric property, even a huge increase in the total production has little effect on the date the peak is reached and decline begins, If we were suddenly to double or triple our energy reserves, we would find plenty of ways to use it: bigger and more comfortable cars, cheaper jet fares and more flights, more electrical appliances, less insulation, throwaway containers, and so on (have doubts? I have three words for you: Sport Utility Vehicle). The sobering reality is that no oil discovery, however large , can forestall the energy crunch very long. Hubbert published a prediction of global oil production in 1969, based on energy use to that time. If the total recoverable oil on earth amounted to 1.35 trillion barrels (a generous estimate in 1969 and 50% more than the total reserves known in 1981), petroleum production would peak and begin to decline about 1990. If the total is half again larger yet, 2.1 trillion barrels (the figure used in the diagrams above), the time of peak production shifts only by ten years, to 2000. We can (and have) flatten out the peak artificially by regulating energy use or raising prices, but the days of unlimited cheap energy are gone with the dinosaurs. Frankly I think the mobile lifestyle we enjoy has a lot of good features; I'd like to see some way to guarantee cheap energy, but fantasy and denial won't bring it about.
We will not run out of oil anytime soon. Oil will be available through the 21st century and probably well after. What will happen is that sometime in the next couple of decades, world demand will exceed production. Oil can only be made to flow through the rocks just so fast, and extracting it too fast can actually shorten the life of an oil field; there may be lots of oil left but so finely dispersed that wells go almost dry. When demand exceeds production the price will go up and stay up.

Some Final Blunt Comments

Americans complain bitterly whenever they have to pay more for something than they think they should (translation, any price that interferes with their buying something else they want). A sense of entitlement pervades American society. Only someone who believes in the Easter Bunny could doubt that oil companies and oil-producing nations try to keep prices up. But consider the following:
  • What have you personally done to deserve access to petroleum at any price? You haven't helped find it, extract it, ship it or refine it. You didn't develop the geological knowledge to locate it, the chemical knowledge to refine it or the engineering knowledge to turn the science into technology. So why, exactly, are you being treated unfairly if those who do the work charge you high prices for it?
  • If you think energy is such a scam, get up off your butt and do something about it. I don't mean the glorified panhandling that we call fund-raising or "educating the public" or political campaigning. If you think there are vast undiscovered reserves out there, study geology and engineering and business, start your own private wildcatting firm (there are lots already - it can be done) and find it!. If you think we could produce it cheaply synthetically, major in chemistry and make it happen, or major in genetics and develop a microbe that can do it. If you think the answer is alternative energy sources, major in physics and engineering and develop them. But don't major in Nondescript Studies and then complain when other people don't do it for you.

References

  • Marie Plummer Minniear, 2000; Forecasting the Permanent Decline in Global Energy Production, Journal of Geoscience Education, v. 48, no. 2, March 2000, p. 130-136.
  • S.W. Carmalt and Bill St. John, 1984; Giant Oil and Gas Fields, in Michael T. Halbouty, ed., Future Petroleum Provinces of the World, American Association of Petroleum Geologists Memoir 40, p. 11-53. Source of the oil field data above.
  • Colin Campbell and Jean H. Laherrere, 1998; The End of Cheap Oil, Scientific American, v. 278, no. 3, pp. 78-83. Contains a good discussion of just how hard it can be to obtain accurate figures of petroleum reserves.
  • Eugene Ayres and Charles A Scarlott, 1952; Energy Sources -- The Wealth of the World, McGraw-Hill, 344p.

Subduction Zones and Orogeny complete notes


What is Orogeny?

Orogeny is the variety of processes that occur during mountain-building, including:
Distinctive Patterns of Deposition
Shallow-water sedimentary rocks on the inner side of the mountain belt, thick deep-water sedimentary rocks in the heart of the mountain belt. Thick accumulations of sandstone and conglomerate accumulate late in the history of the mountain range as it erodes.
Deformation
Folding and thrust-faulting
Metamorphism
Greenschist and amphibolite metamorphism in the core of the range, blueschist metamorphism along its outer edge.
Intrusions
Granitic batholiths are usually associated with orogeny.
Volcanic Activity
Along the crest of the mountain range there is typically a chain of andesite volcanoes.
Oceanic Trenches
Along the outer edge of most currently active mountain belts is a narrow, deep oceanic trench.
Seismic Activity
Shallow great earthquakes along the inner wall of the trench, then deeper earthquakes along a planar zone dipping beneath the mountain range, reaching depths of up to 700 kilometers.

Why Mountains Form

Mountains form at subduction zones. Shown below is a true-scale cross-section of the Andean subduction zone in northern Chile (roughly 25 S).

The vertical change of 15 kilometers in only a few hundred kilometers distance is the largest elevation change on Earth in such a short distance. Plates consist not only of the crust, but about 150 kilometers of the underlying mantle as well. Collectively the crust and associated mantle are termed the lithosphere. Oceanic crust is typically 5 kilometers thick. The continental crust thickens from its normal 40 kilometers to 70 beneath the high Andes. When the descending slab reaches a depth of about 100 kilometers, it begins to melt, causing, directly or indirectly, many of the events associated with mountain-building.


Why Mountains are High

Mountains are high because orogeny shortens and thickens the crust, and isostasy causes the thicker crust to rise. Some of the processes are shown above:
  1. Even uniform materials, when compressed from one direction, tend to expand in the direction of least resistance.
  2. Layered rocks shorten by folding, but the stack of layers also becomes thicker.
  3. Thrust-faulting thickens the crust by stacking slices of crust atop one another.
  4. Intrusions add volume to the crust.
  5. A great deal of magma never invades the crust but accumulates at its base, a process calledunderplating.
  6. Where the crust is heated, thermal expansion causes the rocks to become lighter and more buoyant.

Types of Subduction Zones

Ocean-Ocean

  • Both plates are oceanic crust
  • Because both plates are basaltic, most volcanism is basaltic
  • Initially results in an island chain, but long-continued subduction and accumulation of volcanic rocks and sediments can create a substantial land mass.
  • Examples:
    • Present day: Aleutians, Marianas, Lesser Antilles
    • Past: Isthmus of Panama, Cuba and Greater Antilles?

Ocean-Continent

  • Descending plate is oceanic crust, overriding plate is a continent.
  • The most "typical" orogenic belt
  • Initial volcanism is basaltic, but increased melting and mixing of magma with crustal rocks results in andesite and finally rhyolite volcanism.
  • Examples:
    • Present day: Andes, Indonesia, Japan
    • Past: California Coast Ranges

Continent-Terrane

  • Often continent-ocean subduction will bring a continent into contact with an island arc or small continental fragment.
  • This happens to most orogenic belts eventually.
  • Result is many fault-bounded regions sharply different from adjacent rocks.
  • Examples:
    • Present day: Eastern "tail" of New Guinea.
    • Past: Western North America, China

Continent-Continent

  • Sometimes continent-ocean subduction will bring a continent into contact with another continent.
  • Result is an orogenic belt in the middle of a continent.
  • The two sides of the orogenic belt are separated by a suture marked by blueschist metamorphism, melange, ophiolites and major faults. The rocks on either side of the suture may show quite different histories.
  • Examples:
    • Present day: Alps, Himalaya, Persian Gulf
    • Past: Appalachians, Urals

Anatomy of an Orogenic Belt

Shown here is a simple continent-ocean orogenic belt. We can divide an orogenic belt into parallel zones defined by their deformation, lithology, or metamorphism. These zones may approximately coincide with each other but somewhat overlap, so it's necessary to have distinct names for them.

Structural Zones

The Accretionary Prism

Sediment eroded from the orogenic belt accumulates in the trench and is intensely deformed as the plates converge. Like the wedge of earth ahead of a bulldozer, the sediment thickens until it is capable of resisting further deformation.

The Igneous Arc

When the descending plate reaches about 100 kilometers depth, it begins to melt. Magma invades the crust, creating batholiths and a volcanic mountain chain. The intrusions also produce metamorphism, and by making the crust more ductile, make it easier to deform. This is the belt of greatest deformation, metamorphism and igneous activity.

The Foreland

Here, metamorphism is mild but compression of the crust results in folding and thrust-faulting. Often this deformation is "thin-skinned", meaning that rock layers near the surface become detached from deeper layers much the way a carpet wrinkles when a piece of furniture is pushed over it.
This process is called decollement. Usually the layer where separation occurs is made up of weak rocks like salt, gypsum, or shale.

The Craton

This is the stable interior of the continent. It may be thinly mantled with sedimentary rocks or have large areas of ancient igneous and metamorphic rocks.

Lithologic Zones

The Eugeocline

The rocks of the accretionary prism and much of the igneous arc consist of great thicknesses of immature deep water sediment. Often these rocks show evidence of deposition in an unstable setting, such as evidence of turbidity flows or submarine landslides. This sort of deposit is known as flysch. Such rocks are typical of a continental rise or trench setting. Accompanying these rocks are often submarine volcanic rocks, pillow lavas.

The Miogeocline

The rocks of the foreland are typically shallow-water sedimentary rocks typical of a continental shelf, which become thinner toward the interior of the continent. Igneous rocks are uncommon.
As the mountain belt rises, great thicknesses of sandstone and conglomerate are deposited on its flanks and frequently bury much of the foreland. These rocks are typically shallow-water or terrestrial, often red in color, and are called molasse deposits.

The Platform

The stable interior of the continent will often be covered with thin layers of shallow-water or terrestrial sedimentary rocks. This thinly-mantled region, part of the craton, is the platform

The Shield

Areas where ancient crystalline rocks are exposed over wide areas are called shields. Every continent has at least one shield. The shield and adjacent platform together make up the craton. Driving from Green Bay to Wausau takes you from a platform into a shield.

Metamorphic Zones

One of the best indicators of former subduction is the presence of paired metamorphic belts, a belt of typical Greenschist and Amphibolite metamorphism flanked by a belt of Blueschist metamorphism.

Greenschist-Amphibolite Metamorphism

The rising magma from the descending plate heats the crust, resulting in greenschist and amphibolite metamorphism in the igneous arc. At very high temperatures, rocks become very dehydrated; even muscovite mica breaks down to potassium feldspar and amphibole to pyroxene. This sort of metamorphism, called granulite metamorphism, occurs deep in the crust just about everywhere simply due to the normal geothermal gradient. At 25 degrees per kilometer, the temperature at the base of the crust, 40 kilometers deep, is 1000 degrees C. Of course, unusually intense heating can cause it to occur at shallower levels.

Blueschist Metamorphism

At high pressures but low temperatures, rocks are metamorphosed to blueschist grade. The reason temperatures are abnormally low is that the descending slab is still cool and helps keep adjacent rocks cool as well.
Normally sodium is the most predictable major element; it occurs just about exclusively in plagioclase. At high pressure and low temperature, though, albite feldspar breaks down and forms the pyroxene jadeiteand amphiboles like glaucophane and aegerine. The amphiboles are bluish, hence the term "blueschist"
It's a bit puzzling that there are very few blueschist rocks older than Mesozoic. Possibly older mountain belts have been eroded to depths where temperatures were too high for blueschist metamorphism. Or perhaps, in most orogenic belts these rocks eventually get heated to greenschist grade, and we only see the places where it hasn't happened yet. Some people have suggested that the geothermal gradient was higher in the past, meaning the deep earth was too hot for blueschist metamorphism.

Eclogite Metamorphism

At about 100 kilometers depth, pyroxene, olivine and plagioclase recrystallize to a denser form to produce sodium-bearing pyroxene and garnet. The result is one of the most beautiful of rocks, eclogite, a mass of light green pyroxene enclosing pink garnets.
Note that the boundary of eclogite metamorphism rises upward within the descending slab. This happens because the rocks are relatively cool. High temperatures inhibit the recrystallization of rocks to denser forms because high temperatures cause materials to expand. Thus eclogite metamorphism occurs at shallower depths in the descending slab. The slab in that area is denser than the surrounding mantle, and its greater density assists it in sinking. This mechanism is called slab pull and is one of the driving mechanisms of plate tectonics.

Continental Drift and Plate Tectonics complete notes


Global Problems in Geology

  • Distribution of Continents
  • Mid-ocean Ridges
  • Trenches
  • Orogenic Belts
    • Deformation
    • Metamorphism
    • Volcanism
    • Earthquakes

Continental Drift

  • Frank Taylor (1910)
  • Alfred Wegener (1912) Die Entstehung Der Kontinente Und Ozeane
  • World War II technology for locating submarines
    • Sonar
    • Magnetometers
  • International Geophysical Year (IGY) 1957-58
    • Full extent of Mid-Ocean Ridges
    • Axial Rift Valley along Ridges
    • Thin Sediment in Oceans
    • Young Ocean Floors
    • Geomagnetic Reversals
  • Worldwide Standardized Seismic Network 1963-
    • Developed in part to Support Nuclear Test-Ban Treaty
    • Common Instrument Design
    • Standardized Timekeeping
    • Central Repositories
    • Unprecedented Accuracy in Location

The Confirmation of Continental Drift

The Geomagnetic Reversal Time Scale

Development of the Geomagnetic Reversal Time Scale
The diagram above, based on one by G. Brent Dalrymple, superbly illustrates how science proceeds by successive approximation. In the first five papers, there is general agreement that the magnetic field had its present orientation for the past million years, but disagreement over whether the previous normal period ended 2.0 or 2.5 million years ago.
The second and third papers were published only 13 days apart, far too short a time to re-analyze data, and write and publish a rebuttal. All these workers knew one another and were constantly communicating informally. There was no doubt they were all reporting their results reliably. The question is: why were they getting different results?
The sixth paper shows what was happening. In addition to the long periods ("epochs") of normal or reversed polarity, there are also short periods, or "events" where the magnetic field flips from one orientation to the other and back in a few thousand years. The rest of the papers show the later progress of adding progressively finer details.
It is important to note that only the magnetic field of the Earth flips; 1.5 million years ago, a present-day compass needle would have pointed south rather than north. The rotation axis of the Earth does not flip!

Discovery of Sea-Floor Spreading

sea floor spreadingsea floor spreading

Where Does Ocean Crust Go?

The answer to that question was already on hand. In 1954, Hugo Benioff had published a study of earthquakes beneath ocean trenches. The following three figures are modified from Benioff's original paper.

Benioff zones
One of the trenches Benioff studied was the Japan-Kurile Trench in the North Pacific.

Benioff zones
A cross-section shows how earthquakes lie on a planar zone dipping from the trench beneath the continent.

Benioff zones
Benioff interpreted the dipping zones of earthquakes as giant thrust faults. He did not envision continental drift at the time.
Benioff zones
Once sea-floor spreading was discovered, it was simple to modify Benioff's concept. The dipping seismic zones are great thrust faults, but oceanic crust is moving continuously along them to be recycled in the Earth's interior.

The Worldwide Standardized Seismic Network

The Worldwide Standardized Seismic Network created a global system of seismographs all using common timekeeping standards and sending data to common repositories. This system allowed radical improvements in accuracy of earthquake locations. Instead of showing a diffuse smear of seismicity along the mid-ocean ridges, the system showed that earthquakes were confined to extremely narrow zones along the crest of the ridges. Basically, the new maps showed that the earth consisted of large blocks or plates of crust with little earthquake activity, bounded by narrow zones of high activity.
There is some activity within the plates. If it looks like the U.S. and Western Europe are particularly hard hit, that reflects the concentration of sensitive instruments capable of detecting tiny earthquakes in those regions.
global earthquake locations
plate boundaries
This, of course, was all motivated by a desire to achieve a deeper understanding of the unique planet on which we live. You wish. I have a bridge in Brooklyn you might be interested in. Or, more in keeping with the Internet age, I have $20 million dollars to share if you give me your bank account number so I can deposit it. No, the motivation was to see if anyone was cheating on the Nuclear Test Ban Treaty.
The first maps published showed a cluster of dots in the Sahara Desert. Anyone reading the papers could figure out that those were French nuclear tests (at that time France controlled Algeria). When the scientists analyzing the data included a short note to that effect, all sorts of red lights and sirens went off in the Pentagon and the State Department, and the note was removed. Meanwhile, every geologist in the world heard the story. You have to wonder what the Pentagon and the State Department accomplished (their children and grandchildren are now in charge of Homeland Security.)

Plate Tectonics

Overview of plate tectonics
The diagram above, from a 1969 paper by Isaacs, Oliver and Sykes, shows the different types of plate interaction
  • Crust of Earth Consists of Rigid Moving Plates
  • Plates Can-
    • Move Apart
      New Crust Created
    • Slide past Each Other
      Strike Slip Faults
    • Converge on Each Other
      Crust Consumed
  • Continents Passive
    • Deformation at Edges
    • Fragmentation
  • Ocean Basins Active
    • Crust Created at Ridges
    • Crust Consumed in Trenches
    • Continental Crust Not Consumed
      • Continents 3900 My
      • Oceans 200 My
    • Recycling of Oceanic Crust
      • Chemical Evoluation of Earth
      • No Old Oceanic Crust
    • Probable Driving Mechanism is Convection
      convection 

Explanatory Power

  • Physiography of Ocean Basins
    • Ridges
    • Abyssal Plains
    • Trenches
    • Seamount Chains
  • Location & Depth of Earthquakes
  • Location & Types of Vulcanism
  • Formation of Mountain Chains
  • Contributes to Explaining
    • Igneous Rock Genesis
    • Paleoclimate
    • Paleoecology
    • Resource Genesis
    • Eustatic Sea Level Changes
  • Quantitative Power - Geometrical Rules
    • Plates Rigid
    • Change Shape in Limited Ways
    • Move on Sphere

Plate Tectonics Cannot Yet Explain

  • Tectonics of Earliest Earth
  • Location of Many Small Fragments
  • Future Plate Motions
  • Global Pattern of Plates (Is there a geometrical pattern?)
  • How and where Plates will Fragment
  • Details of Driving Mechanism

Reconstructing Plate Motions

  • Can provide Exact Reconstruction
    • Continental Fit
      continental reconstruction
      This pioneering computer reconstruction, done in 1965, is so good that new data have had almost no effect on it. The actual edge of the continental crust is buried under the edge of the continental shelf and the submarine contour used in the reconstruction is only an approximation. Minor gaps and overlaps are expected and not a concern.
    • Magnetic Stripes
  • Can Provide Latitude Only
    • Paleomagnetism
    • Paleoclimate
  • Can Give Loose Indications of Plate Proximity
    • Paleoecology
    • Sequence of Collisions

Geology of Plate Margins

Spreading Centers

Transform Faults

Subduction Zones and Orogeny

Terrane Accretion

Hot Spots

Hawaii Hot spot tracks

History of Continental Movements

Rodinia and Other pre-Pangaea Supercontinents

Plate Tectonics and Regional Geology

Closing of the Tethys

The North Pacific and the West Coast of North America

Sea-floor spreading creates symmetrical patterns on both plates. Thus, if one plate is entirely subducted, it is still possible to reconstruct some of its history from the surviving plate. This is the case off the west coast of North America, where a now-vanished plate can be reconstructed.