Relationship of structural development and Cenozoic sedimentation, northern Gulf of Mexico
Abstract
Development of structure in the northern Gulf of Mexico, mainly listric faulting and salt features, is directly related to Cenozoic sedimentation. Essentially all oil and gas production in this region occurs in structural features resulting from faulting and/or salt movement. A thick section of continental shallow-water sediments rimming the entire Gulf of Mexico was deposited during overall Gulf subsidence in Mesozoic time. Very little sedimentation took place in the central Gulf, so that, at the close of the Mesozoic the central Gulf probably was of abyssal depths. Cenozoic sedimentation surpassed the rate of subsidence causing sediments to prograde across the Mesozoic shelf margin, with greatest deposition occurring gulfward of this margin. These depocenters or areas of thickest sedimentation prograded gulfward throughout time (in response to sediment supply) and migrated northeastward from south Texas to south Louisiana. Listric or growth faults that formed contemporaneously with deposition are a common structural feature developed during Cenozoic sedimentation. These features are apparently caused by differential loading of higher density sandstones on prodelta shales near the shelf margin. In those areas underlain by thicker salt, such as the Miocene and younger depocenters, there is greater involvement of salt in growth-fault development. Salt features, the othermore »
- Authors:
- Publication Date:
- Research Org.:
- Chevron Inc., New Orleans, LA
- OSTI Identifier:
- 5782306
- Report Number(s):
- CONF-850322-
Journal ID: CODEN: AAPGB
- Resource Type:
- Conference
- Journal Name:
- Am. Assoc. Pet. Geol., Bull.; (United States)
- Additional Journal Information:
- Journal Volume: 69:2; Conference: American Association of Petroleum Geologists annual meeting, New Orleans, LA, USA, 25 Mar 1985
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 02 PETROLEUM; GULF OF MEXICO; GEOLOGIC HISTORY; GEOLOGIC TRAPS; SEDIMENTATION; GEOLOGIC FAULTS; PETROLEUM DEPOSITS; SALT DEPOSITS; ATLANTIC OCEAN; CARIBBEAN SEA; GEOLOGIC DEPOSITS; GEOLOGIC FRACTURES; GEOLOGIC STRUCTURES; MINERAL RESOURCES; RESOURCES; SEAS; SURFACE WATERS; 020200* - Petroleum- Reserves, Geology, & Exploration
Citation Formats
Humphris, Jr, C C. Relationship of structural development and Cenozoic sedimentation, northern Gulf of Mexico. United States: N. p., 1985.
Web.
Humphris, Jr, C C. Relationship of structural development and Cenozoic sedimentation, northern Gulf of Mexico. United States.
Humphris, Jr, C C. 1985.
"Relationship of structural development and Cenozoic sedimentation, northern Gulf of Mexico". United States.
@article{osti_5782306,
title = {Relationship of structural development and Cenozoic sedimentation, northern Gulf of Mexico},
author = {Humphris, Jr, C C},
abstractNote = {Development of structure in the northern Gulf of Mexico, mainly listric faulting and salt features, is directly related to Cenozoic sedimentation. Essentially all oil and gas production in this region occurs in structural features resulting from faulting and/or salt movement. A thick section of continental shallow-water sediments rimming the entire Gulf of Mexico was deposited during overall Gulf subsidence in Mesozoic time. Very little sedimentation took place in the central Gulf, so that, at the close of the Mesozoic the central Gulf probably was of abyssal depths. Cenozoic sedimentation surpassed the rate of subsidence causing sediments to prograde across the Mesozoic shelf margin, with greatest deposition occurring gulfward of this margin. These depocenters or areas of thickest sedimentation prograded gulfward throughout time (in response to sediment supply) and migrated northeastward from south Texas to south Louisiana. Listric or growth faults that formed contemporaneously with deposition are a common structural feature developed during Cenozoic sedimentation. These features are apparently caused by differential loading of higher density sandstones on prodelta shales near the shelf margin. In those areas underlain by thicker salt, such as the Miocene and younger depocenters, there is greater involvement of salt in growth-fault development. Salt features, the other major type of producing structure, are developed by salt movement as a direct response to Cenozoic sediment loading. Initiation of salt movement is believed to be due to differential loading of prograding sediments. Further salt movement and structural development are completely dependent on continued sedimentation.},
doi = {},
url = {https://www.osti.gov/biblio/5782306},
journal = {Am. Assoc. Pet. Geol., Bull.; (United States)},
number = ,
volume = 69:2,
place = {United States},
year = {Fri Feb 01 00:00:00 EST 1985},
month = {Fri Feb 01 00:00:00 EST 1985}
}