Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska
The Late Jurassic through Cretaceous geological history of the Chukchi Shelf and adjacent onshore Alaska is the focus of an integrated study using seismic, well, outcrop and geochronological data across a 150,000 km2 area. This work suggests several fundamental linkages between tectonics and basin e...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.666.9016 2023-05-15T15:46:59+02:00 Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska David W. Houseknecht The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.666.9016 http://alaskageology.org/documents/14/February+2014+Newsletter.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.666.9016 http://alaskageology.org/documents/14/February+2014+Newsletter.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://alaskageology.org/documents/14/February+2014+Newsletter.pdf text ftciteseerx 2016-01-08T17:08:28Z The Late Jurassic through Cretaceous geological history of the Chukchi Shelf and adjacent onshore Alaska is the focus of an integrated study using seismic, well, outcrop and geochronological data across a 150,000 km2 area. This work suggests several fundamental linkages between tectonics and basin evolution, and clarifies offshore-onshore relations. Inherited tectonic elements influenced Late Jurassic and subsequent structural response to stresses related to the Chukotka (Late Jurassic through Cretaceous) and Brooks Range (Early Cretaceous and Tertiary) orogenies, as well as Beaufortian and Brookian sediment routing and accumulation patterns. Particularly important elements include the Chukchi Platform, a long-lived and high-standing block of pre-Mississippian rocks beneath the western Chukchi shelf; Hanna Trough, a Late Paleozoic failed rift system that bisects the shelf from north to south; and Alaska rift shoulder, a Jurassic and younger uplift related to opening of the Amerasia Basin. Contractional deformation, apparently related to the Chukotka orogeny, spanned at least the Late Jurassic through Late Cretaceous on the Chukchi Shelf. The initial pulse of contraction is evidenced by a series of en-echelon, north-south trending reverse or transpressional faults, which display up to 1 km of structural relief and root into older normal faults associated with the Hanna Trough. These inversion structures likely reflect maximum stress oriented obliquely to relict normal faults. Petroleum-prospective Upper Jurassic – Neocomian strata display eastward growth across the Text Brooks Range Chukchi Chukotka Alaska Unknown Chukchi Shelf ENVELOPE(-169.167,-169.167,70.550,70.550) Amerasia Basin ENVELOPE(-170.000,-170.000,80.000,80.000) |
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ftciteseerx |
language |
English |
description |
The Late Jurassic through Cretaceous geological history of the Chukchi Shelf and adjacent onshore Alaska is the focus of an integrated study using seismic, well, outcrop and geochronological data across a 150,000 km2 area. This work suggests several fundamental linkages between tectonics and basin evolution, and clarifies offshore-onshore relations. Inherited tectonic elements influenced Late Jurassic and subsequent structural response to stresses related to the Chukotka (Late Jurassic through Cretaceous) and Brooks Range (Early Cretaceous and Tertiary) orogenies, as well as Beaufortian and Brookian sediment routing and accumulation patterns. Particularly important elements include the Chukchi Platform, a long-lived and high-standing block of pre-Mississippian rocks beneath the western Chukchi shelf; Hanna Trough, a Late Paleozoic failed rift system that bisects the shelf from north to south; and Alaska rift shoulder, a Jurassic and younger uplift related to opening of the Amerasia Basin. Contractional deformation, apparently related to the Chukotka orogeny, spanned at least the Late Jurassic through Late Cretaceous on the Chukchi Shelf. The initial pulse of contraction is evidenced by a series of en-echelon, north-south trending reverse or transpressional faults, which display up to 1 km of structural relief and root into older normal faults associated with the Hanna Trough. These inversion structures likely reflect maximum stress oriented obliquely to relict normal faults. Petroleum-prospective Upper Jurassic – Neocomian strata display eastward growth across the |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
David W. Houseknecht |
spellingShingle |
David W. Houseknecht Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska |
author_facet |
David W. Houseknecht |
author_sort |
David W. Houseknecht |
title |
Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska |
title_short |
Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska |
title_full |
Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska |
title_fullStr |
Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska |
title_full_unstemmed |
Late Jurassic through Cretaceous Tectonics and Basin Evolution, Chukchi Shelf and Northwestern Alaska |
title_sort |
late jurassic through cretaceous tectonics and basin evolution, chukchi shelf and northwestern alaska |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.666.9016 http://alaskageology.org/documents/14/February+2014+Newsletter.pdf |
long_lat |
ENVELOPE(-169.167,-169.167,70.550,70.550) ENVELOPE(-170.000,-170.000,80.000,80.000) |
geographic |
Chukchi Shelf Amerasia Basin |
geographic_facet |
Chukchi Shelf Amerasia Basin |
genre |
Brooks Range Chukchi Chukotka Alaska |
genre_facet |
Brooks Range Chukchi Chukotka Alaska |
op_source |
http://alaskageology.org/documents/14/February+2014+Newsletter.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.666.9016 http://alaskageology.org/documents/14/February+2014+Newsletter.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766381796597956608 |