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Paleokarst
  • Language: en
  • Pages: 422

Paleokarst

Landscapes of the past have always held an inherent fascination for ge ologists because, like terrestrial sediments, they formed in our environment, not offshore on the sea floor and not deep in the subsurface. So, a walk across an ancient karst surface is truly a step back in time on a surface formed open to the air, long before humans populated the globe. Ancient karst, with its associated subterranean features, is also of great scientific interest because it not only records past exposure of parts of the earth's crust, but preserves information about ancient climate and the movement of waters in paleoaquifers. Because some paleokarst terranes are locally hosts for hydrocarbons and base me...

Carbonate Petroleum Reservoirs
  • Language: en
  • Pages: 587

Carbonate Petroleum Reservoirs

The case history approach has an impressive record of success in a variety of disciplines. Collections of case histories, casebooks, are now widely used in all sorts of specialties other than in their familiar application to law and medicine. The case method had its formal beginning at Harvard in 1871 when Christopher Lagdell developed it as a means of teaching. It was so successful in teaching law that it was soon adopted in medical education, and the col lection of cases provided the raw material for research on various diseases. Subsequently, the case history approach spread to such varied fields as busi ness, psychology, management, and economics, and there are over 100 books in print th...

Carbonate Sedimentology and Petrology
  • Language: en
  • Pages: 160

Carbonate Sedimentology and Petrology

None

Carbonate Depositional Environments
  • Language: en
  • Pages: 694

Carbonate Depositional Environments

  • Type: Book
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  • Published: 1983
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  • Publisher: AAPG

This is the book you need to improve your interpretations of carbonates. Using a systematic treatment of the entire subject of carbonate depositional environments, this unique book is specifically designed for use by the non-specialist -- the petroleum geologist or field geologist -- who uses carbonate depositional environments in facies reconstructions and environmental intepretations. This classic work, covering settings from non-marine to deep water, focuses on the recognition of depositional environments with extenive use of color diagrams and photographs of sedimentary structures and facies assemblages. Although the ultimate purpose of this text is to improve exploration for oil, gas, a...

Uranium Occurrences in Bucks County, Pennsylvania, and Hunterdon County, New Jersey
  • Language: en
  • Pages: 72
A Color Guide to the Petrography of Carbonate Rocks
  • Language: en
  • Pages: 459

A Color Guide to the Petrography of Carbonate Rocks

  • Type: Book
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  • Published: 2003
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  • Publisher: AAPG

None

The American Association of Petroleum Geologists Bulletin
  • Language: en
  • Pages: 2028

The American Association of Petroleum Geologists Bulletin

  • Type: Book
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  • Published: 1973
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  • Publisher: Unknown

None

Bulletin of the Southwestern Association of Petroleum Geologists
  • Language: en
  • Pages: 360

Bulletin of the Southwestern Association of Petroleum Geologists

  • Type: Book
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  • Published: 1973
  • -
  • Publisher: Unknown

None

Abstracts of North American Geology
  • Language: en
  • Pages: 1060

Abstracts of North American Geology

  • Type: Book
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  • Published: 1969
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  • Publisher: Unknown

None

Subsurface Geology of a Prograding Carbonate Platform Margin, Great Bahama Bank
  • Language: en
  • Pages: 290

Subsurface Geology of a Prograding Carbonate Platform Margin, Great Bahama Bank

This volume will be of special interest to carbonate sedimentologists, geochemists, petroleum geologists, engineers, and seismologists. It addresses fundamental aspects of prograding carbonate platforms in a Neogene example from Great Bahama Bank. A remarkable seismic profile, which imaged the prograding margin, provided the seismic stratigraphic framework. Two continuouslycored and logged borings on the profile produced the ground truth for testing and characterizing processes: lithologies and ages of sequence boundaries; influence of sea level fluctuations on progradation, controls on impedance contrasts in carbonates; fluid flow through the submerged margin; log responses of different lithologies; and the origin, ages and depositional environments of the platform top and prograding clinothems. The new findings on diagenesis are of special interest, including complete mineral stabilization in seawater, early burial dolomitization related to sequence boundaries and how diagenesis controls sonic velocity and permeability.