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Sedimentology and sedimentary geochemistry of the Eagle Ford Group, Texas

Abstract:

The Eagle Ford Group is an organic-rich succession of rhythmically interbedded packstones and wackestones, deposited in the southern Western Interior Seaway during the Cenomanian-Turonian of the Upper Cretaceous. Recent investigations have suggested that either eustatic sea level change, astronomical forcings, change in primary productivity and dilution, or changes in local and global benthic oxygenation may be responsible for the Eagle Ford Groups lithological and geochemical variat...

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Division:
MPLS
Department:
Earth Sciences
Role:
Author

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Role:
Supervisor
Role:
Supervisor
Role:
Supervisor
Type of award:
DPhil
Level of award:
Doctoral
Awarding institution:
University of Oxford
UUID:
uuid:79a42ac1-1672-493b-9781-bfb07b21af9e
Deposit date:
2018-10-24

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