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The AAPG/Datapages Combined Publications Database

Showing 43,524 Results. Searched 196,128 documents.

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Stratigraphic Traps in Southeastern Louisiana

The New Orleans Geological Society Study Group

GCAGS Transactions

... of deep stratigraphic data. Originally thought to be a fault trap, it now appears to be a purely stratigraphic phenomenon. The following facts are known...

1963

Petroleum Geology of Central Sedimentary Basin of Uruguay

Victor Oppenheim

AAPG Bulletin

... Brazil, continues southward as a wide plateau in Uruguay with an east-facing escarpment 250-300 meters high, extending as a wide trap plateau west...

1935

A Bibliography of Rocky Mountain Oil and Gas Fields

Editor: Mark W. Longman, Editor: Michael S. Johnson

Rocky Mountain Association of Geologists

... trap: AAPG Bulletin, v. 41, no. 5, p. 823-838. Cottonwood Creek (WY) Pedry, J.J., 1975a, Tensleep fault trap, Cottonwood Creek Field, Washalue County...

1999

Superficial Structures and Stress Regimes of the Downgoing Plate Associated with Subduction-Collision in the Central New Hebrides Arc (Vanuatu)

Robert V. Burne, Jean-Yves Collot, Jacques Daniel

Circum Pacific Council Publications

... the plates and subduction is mainly controlled by creep. Between the North D'Entrecasteaux Ridge and latitude 17 S, a compressional stress regime...

1988

Units of the East Kuban Downwarp and Their Oil-Gas Productivity

M. R. Pustil’nikov, G. A. Aleksin, N. Ye. Mitin

Petroleum Geology: A Digest of Russian Literature

... pericline of the downwarp is bounded by a transverse fault which runs along the east border of the Novo-Minsko-Kanelov anticlinal zone. See Fig. 1. The trend...

1964

Geothermal Characteristics of the Emba Region

D. A. Dzhangir’yantz

Petroleum Geology: A Digest of Russian Literature

... of temperature in the subsurface waters of the upper Albian and Cenomanian; this is due to of heat from depth along fault zones. See Fig. 3. Figure 3. Map...

1965

Fracture Pressure Predictions in Highly Depleted Reservoir: An Approach to Prevent Mud Losses while Drilling in the Mature Tunu Field

Dhanny Fadlan, Roni Herdiyanto, Baginda Saragih, Yasinto Priastomo, Rio Sitorus, Roy Lesmana

Indonesian Petroleum Association

... in depleted sandstone and not due to a fault and/or massive limestone which may cause mud losses in Tunu Field. Poisson’s ratio is obtained from back...

2016

Timing and Mechanism of the Opening of the Western Black Sea Basin, #30152 (2011)

Okan Tüysüz

Search and Discovery.com

..., a compressional regime started to affect the Western Pontides. This compressional regime is still active in the eastern part of the Western Black Sea...

2011

Seismic Stratigraphy of Eocene Beriun Sands of West Bungalun, East Kalimantan, Indonesia: A Contribution to the Paleogene Stratigraphical Knowledge of the Kutei Basin

Awang Harun Satyana, Elan Biantoro

Indonesian Petroleum Association

... Oligocene, regressive deltaic sedimentation began and became the dominant depositional regime in the basin. These Neogene deltaic deposits constitute...

1996

Defining Kofiau Sub-Basin as the Deepest Part of Salawati Basin using Satellite Gravity Interpretation Approach

Anggoro P. Kurniawan, Boko Nurdiyanto Suwardi, Fatrial Bahesti, Soffan M. Hadi, Hendarsyah, Agung Prasetyo

Indonesian Petroleum Association

... is defined as a Cenozoic foreland basin with a wedge top area on the northern part, bounded by the Sorong Fault Zone, and an E-W-trending elongate foredeep...

2018

Evidence for Recent Migration of Geopressured Fluids along Faults in Eugene Island, Block 330, Offshore Louisiana, from Estimates of Pore Water Salinity

Guichang Lin, Jeffrey A. Nunn

GCAGS Transactions

... Salinity Guichang Lin, Jeffrey A. Nunn 1997 Vol. 47 (1997), We estimated the pore water salinity of reservoir sands near a major fault in the Eugene...

1997

Lessons Learned from the Exploration of Naturally Fractured Basement Reservoir, A Case Study in Indonesia

Yudha Risnandar Sinulingga, Faisal Siddiq, Arii Ardjuna, Sumaryana, Budi R. Permana

Indonesian Petroleum Association

..., conduct tectonic evaluation for Paleo Basement High, Poly-Phase Tectonics, Fault Damage Zone, Maximum Peak/Arch Area, Fault Abundance, and Critical...

2024

Petroleum Systems of the Neiva Area, Upper Magdalena Valley, Colombia: Chapter 30: Part V. Case Studies--Western Hemisphere

Jaime Buitrago

AAPG Special Volumes

... of a faulted anticline, a fault and a subunconformity, or just a fault trap. The fields producing from the Honda Group also have a stratigraphic...

1994

Origin and Accumulation of Oil: Part III. Migration and Accumulation of Petroleum

Frank R. Clark

AAPG Special Volumes

... is sparsely and widely disseminated organic matter in shales and limestones, and that free oil migrates long distances to its final trap, fails to satisfy...

1934

Oil-Gas Prospects of the North Zone of Small-Scale Folding of the Donets Basin

A. T. Murich

Petroleum Geology: A Digest of Russian Literature

... properties in units of the Carboniferous in the zone of small-scale folding of the Donets Basin. The presence of sectors with a stagnant water regime...

1973

Shtokmanov-Lunin Mega-Saddle - Highly Favorable Type of Structure of Barents-Kara Platform

I. S. Gramberg, O. I. Suprunenko, V. Shipel’kevich

Petroleum Geology: A Digest of Russian Literature

... and marks a re-structuring of the geodynamic regime with transition from predominantly carbonate deposition to clastic deposition almost everywhere...

2002

Relationships Between Pore Pressure, Stresses, and Present-Day Geodynamics in the Scotian Shelf, Offshore Eastern Canada

N. A. Yassir , J. S. Bell

AAPG Bulletin

... eastern Canada: Bulletin of Canadian Petroleum Geology, v. 37, no. 3, p. 358-364. Bell, J. S., 1990a, The stress regime of the Scotian Shelf, offshore...

1994

ABSTRACT: Interplay between Tectonics and Sedimentation in the Lower Pliocene Fill of the Crotone Basin, Southern Italy; #90013 (2003)

ZECCHIN MASSIMO, DONATELLA MELLERE, FRANCESCO, MASSARI, GIACOMO PROSSER

Search and Discovery.com

... deposition of Zinga 2 and Zinga 3 sequences The deposition of Zinga 2 and Zinga 3 sequences was characterized by an accentuation of the extensional regime...

2003

The Wind River Range, Wyoming: An Overview

D. L. Blackstone Jr.

Wyoming Geological Association

... thrust fault under a compressional stress regime. Deformation began approximately 66 Ma (Lancian) and terminated 51 Ma (Bridgerian). The fault plane...

1993

Rift Border System: The Interplay Between Tectonics and Sedimentation in the Reconcavo Basin, Northeastern Brazil

Luciano P. Magnavita, Hercules T. F. da Silva

AAPG Bulletin

... fault system at marker 50 level (Figure 12). The time correlated with marker 50 also stresses a drastic change in the depositional regime because...

1995

Bedrock Geology of the Dempster Lateral

D. K. Norris

CSPG Special Publications

... and east of the Tintina Fault: 25th Intern. Geol. Cong., Abstracts, v. 3, p. 690-692. Norris, D. K., 1977, Geology and Hydrocarbon Resources, Northern...

1980

Wasatch Plateau Gas Fields, Utah

Paul T. Walton

AAPG Bulletin

...: A fault segment on the east side of the Gordon Creek structure (Fig. 4) is large enough to be an effective trap for gas, but, being on the east side...

1955

Geology of the Eastern Margin of the Indian Subcontinent

Y. S. N. Rao

Southeast Asia Petroleum Exploration Society (SEAPEX)

... of basaltic volcanism contemporaneous with the Deccan Trap eruption. However, in an exploratory well drilled recently in the Gulf of Mannar, dolerites...

1980

A Tale of Two Fields: Surubi and Paloma, Mamore Block Bolivia

Jeffrey M. Dunleavy

Asociación Colombiana de Geólogos y Geofisicos del Petróleo (ACGGP)

... trap, as the fault cut the structure, creating a separate field which exhibited original reservoir pressure when discovered. The second phase...

2000

Chapter 4: Adding New Reserves and Production in Giant Fields

John S. Sneider, Michael A. Rosen, Dorothy E. Ballentine

AAPG Special Volumes

... of the Cretaceous Natih Formation (Figure 31). The trap is a tilted fault block more than 35 km2 (~14 mi2) in area, 500–700 m (~1600–2300 ft) below the surface...

2021

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