Author: Scott Brian Blount
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 354
Book Description
Depositional and Diagenetic History of the Hosston Formation (Travis Peak), Nuevo Leon Group, Trawick Field, Nacogdoches County, Texas
Author: Scott Brian Blount
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 354
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 354
Book Description
Petroleum Abstracts
Author:
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 840
Book Description
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 840
Book Description
Transactions
Author: Gulf Coast Association of Geological Societies
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 706
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 706
Book Description
Comprehensive Index of the Publications of the ... Association
Author: American Association of Petroleum Geologists
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 496
Book Description
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 496
Book Description
Memorials - The Geological Society of America
Author: Geological Society of America
Publisher:
ISBN:
Category : Geologists
Languages : en
Pages : 130
Book Description
Publisher:
ISBN:
Category : Geologists
Languages : en
Pages : 130
Book Description
Comprehensive Index of Publications of the American Association of Petroleum Geologists
Author: American Association of Petroleum Geologists
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 496
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 496
Book Description
Bibliography and Index of Geology
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1440
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1440
Book Description
Geoscience Documentation
Author:
Publisher:
ISBN:
Category : Earth sciences
Languages : en
Pages : 364
Book Description
Publisher:
ISBN:
Category : Earth sciences
Languages : en
Pages : 364
Book Description
Petroleum Abstracts. Literature and Patents
Author:
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 1656
Book Description
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 1656
Book Description
The Travis Peak (Hosston) formation
Author: Robert J. Finley
Publisher:
ISBN:
Category : Formations (Geology)
Languages : en
Pages : 233
Book Description
The Travis Peak (Hosston) formation constitutes a 1,000- to 5,000-ft-thick clastic wedge that formed two major depocenters along the north flank of the Gulf Coast Basin. The depocenters were dominated by fluvial-deltaic facies. A delta-fringe facies, including tidal flat and nearshore shallow-margin shelf facies, formed around the margins of the clastic wedge. These marginal-marine deposits within the upper Travis Peak are the most important productive facies of the formation within a nine-county area in East Texas. Sandstones in the Travis Peak are mineralogically mature. Low permeability and occlusion of porosity is primarily due to quartz overgrowths, authigenic clay, ankerite, and reservoir bitumen, a high-molecular-weight hydrocarbon residue. Within six Travis Peak gas fields in East Texas, porosity ranges from 8 to 11 percent and water saturation ranges from 28 to 44 percent within intervals of net pay. The permeability-thickness product is low in the southern part of the study area and increases toward the north. Upper limits of permeability range from 0.074 md (median value) to 0.084 md (thickness-weighted average), based on well tests that postdate fracture treatment. Within Chapel Hill field, three reservoir sandstone types were defined; sandstones with greatest lateral continuity were deposited as sandy tidal flats, including associated channel sandstones that trend northwest. Lower energy tidal-flat deposition is characterized by increased mud content of sandstones, and low marine transgression resulted in deposition of mudstone and muddy limestone.
Publisher:
ISBN:
Category : Formations (Geology)
Languages : en
Pages : 233
Book Description
The Travis Peak (Hosston) formation constitutes a 1,000- to 5,000-ft-thick clastic wedge that formed two major depocenters along the north flank of the Gulf Coast Basin. The depocenters were dominated by fluvial-deltaic facies. A delta-fringe facies, including tidal flat and nearshore shallow-margin shelf facies, formed around the margins of the clastic wedge. These marginal-marine deposits within the upper Travis Peak are the most important productive facies of the formation within a nine-county area in East Texas. Sandstones in the Travis Peak are mineralogically mature. Low permeability and occlusion of porosity is primarily due to quartz overgrowths, authigenic clay, ankerite, and reservoir bitumen, a high-molecular-weight hydrocarbon residue. Within six Travis Peak gas fields in East Texas, porosity ranges from 8 to 11 percent and water saturation ranges from 28 to 44 percent within intervals of net pay. The permeability-thickness product is low in the southern part of the study area and increases toward the north. Upper limits of permeability range from 0.074 md (median value) to 0.084 md (thickness-weighted average), based on well tests that postdate fracture treatment. Within Chapel Hill field, three reservoir sandstone types were defined; sandstones with greatest lateral continuity were deposited as sandy tidal flats, including associated channel sandstones that trend northwest. Lower energy tidal-flat deposition is characterized by increased mud content of sandstones, and low marine transgression resulted in deposition of mudstone and muddy limestone.