The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential

Seismic stratigraphic and seismic fault evidence both show that the Central Chukchi basin is a north-trending, fault-controlled basin, which developed at the beginning of early Mississippian time. About 20 km thickness of sediments have been deposited in the basin. Using a simple flexural model a se...

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Published in:Energy Exploration & Exploitation
Main Authors: Lerche, I., Cao, S., Tang, J., Liu, J.
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 1993
Subjects:
Online Access:http://dx.doi.org/10.1177/0144598793011003-403
https://journals.sagepub.com/doi/pdf/10.1177/0144598793011003-403
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spelling crsagepubl:10.1177/0144598793011003-403 2024-10-20T14:08:01+00:00 The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential Lerche, I. Cao, S. Tang, J. Liu, J. 1993 http://dx.doi.org/10.1177/0144598793011003-403 https://journals.sagepub.com/doi/pdf/10.1177/0144598793011003-403 en eng SAGE Publications https://journals.sagepub.com/page/policies/text-and-data-mining-license Energy Exploration & Exploitation volume 11, issue 3-4, page 235-283 ISSN 0144-5987 2048-4054 journal-article 1993 crsagepubl https://doi.org/10.1177/0144598793011003-403 2024-09-24T04:14:01Z Seismic stratigraphic and seismic fault evidence both show that the Central Chukchi basin is a north-trending, fault-controlled basin, which developed at the beginning of early Mississippian time. About 20 km thickness of sediments have been deposited in the basin. Using a simple flexural model a series of 3-dimensional basement motion patterns with time was produced. From these characteristic patterns two stages of basement evolution can be recognized: the first is basement subsidence controlled by regional extensional fault systems during the period from early Mississippian to later Jurassic: the second stage is basement evolution as two nearly separate blocks from the beginning of Early Cretaceous. The west block development is related to reactivation of the old fault system, while the subsidence of the east block is caused by tectonism and associated sediment loading due to progressive thrusting northward of the Brooks Range. Quantitative basin modeling techniques show that many uncertainties occur when applying mathematical and computer models to simulate a sedimentary basin, especially in a frontier area where only limited data are available. In this study, quantitative basin modeling techniques applied to the Chukchi Sea Planning Area, Alaska, demonstrate how uncertainty can be handled. The Chukchi Sea Planning Area encompasses about 127,000 square kilometers of the northwestern Alaska continental shelf and lies offshore of the Natural Petroleum Reserve in Alaska. Only seismic data and a few remote onshore wells are available in the Planning Area. Compared with the North Slope of Alaska, the Planning Area has had a significantly different structural history. In addition, most of the strata in the Area are currently thermally mature to overmature and in the stage of generating dry gas. The prospective areas for oil are the margins of the central Chukchi Basin, such as the Chukchi platform, Herald Arch and northeast part of the basin. Article in Journal/Newspaper Brooks Range Chukchi Chukchi Sea north slope Alaska SAGE Publications Chukchi Sea Energy Exploration & Exploitation 11 3-4 235 283
institution Open Polar
collection SAGE Publications
op_collection_id crsagepubl
language English
description Seismic stratigraphic and seismic fault evidence both show that the Central Chukchi basin is a north-trending, fault-controlled basin, which developed at the beginning of early Mississippian time. About 20 km thickness of sediments have been deposited in the basin. Using a simple flexural model a series of 3-dimensional basement motion patterns with time was produced. From these characteristic patterns two stages of basement evolution can be recognized: the first is basement subsidence controlled by regional extensional fault systems during the period from early Mississippian to later Jurassic: the second stage is basement evolution as two nearly separate blocks from the beginning of Early Cretaceous. The west block development is related to reactivation of the old fault system, while the subsidence of the east block is caused by tectonism and associated sediment loading due to progressive thrusting northward of the Brooks Range. Quantitative basin modeling techniques show that many uncertainties occur when applying mathematical and computer models to simulate a sedimentary basin, especially in a frontier area where only limited data are available. In this study, quantitative basin modeling techniques applied to the Chukchi Sea Planning Area, Alaska, demonstrate how uncertainty can be handled. The Chukchi Sea Planning Area encompasses about 127,000 square kilometers of the northwestern Alaska continental shelf and lies offshore of the Natural Petroleum Reserve in Alaska. Only seismic data and a few remote onshore wells are available in the Planning Area. Compared with the North Slope of Alaska, the Planning Area has had a significantly different structural history. In addition, most of the strata in the Area are currently thermally mature to overmature and in the stage of generating dry gas. The prospective areas for oil are the margins of the central Chukchi Basin, such as the Chukchi platform, Herald Arch and northeast part of the basin.
format Article in Journal/Newspaper
author Lerche, I.
Cao, S.
Tang, J.
Liu, J.
spellingShingle Lerche, I.
Cao, S.
Tang, J.
Liu, J.
The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential
author_facet Lerche, I.
Cao, S.
Tang, J.
Liu, J.
author_sort Lerche, I.
title The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential
title_short The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential
title_full The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential
title_fullStr The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential
title_full_unstemmed The Chukchi Sea Planning Area, Alaska: Structural Development, Basin Analysis and Hydrocarbon Potential
title_sort chukchi sea planning area, alaska: structural development, basin analysis and hydrocarbon potential
publisher SAGE Publications
publishDate 1993
url http://dx.doi.org/10.1177/0144598793011003-403
https://journals.sagepub.com/doi/pdf/10.1177/0144598793011003-403
geographic Chukchi Sea
geographic_facet Chukchi Sea
genre Brooks Range
Chukchi
Chukchi Sea
north slope
Alaska
genre_facet Brooks Range
Chukchi
Chukchi Sea
north slope
Alaska
op_source Energy Exploration & Exploitation
volume 11, issue 3-4, page 235-283
ISSN 0144-5987 2048-4054
op_rights https://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/0144598793011003-403
container_title Energy Exploration & Exploitation
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