Show simple item record

dc.contributor.advisorSaltzman, Matthew R.
dc.creatorCramer, Brad
dc.date.accessioned2009-08-19T13:53:32Z
dc.date.available2009-08-19T13:53:32Z
dc.date.issued2002-06
dc.identifier.urihttp://hdl.handle.net/1811/38832
dc.description.abstractMethane has become an attractive answer for the anomalous and has recently been used to explain numerous carbonates, especially mud mounds, in the rock record. The criteria for recognizing methane seeping from the sea floor (cold seeps) have not been standardized, resulting in a variety of arguments asserting the influence of methane. This study is an attempt to classify six criteria which would allow for the positive identification of a fossil cold seep; independent of age, geologic setting, depositional depth, or lithology.en_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. Department of Geological Sciences Senior Theses; 2002en_US
dc.subjectcarbonate mud moundsen_US
dc.subjectcold seepsen_US
dc.subjectpaleoenvironmenten_US
dc.subjectmethaneen_US
dc.subjectanaerobic methane oxidationen_US
dc.subjectsulfate reductionen_US
dc.subjectcarbon isotopesen_US
dc.subjectmethanogenesisen_US
dc.subjectsyntrophicen_US
dc.titleAn Integrated Approach to Recognizing Fossil Cold Seeps: Methodology and Applicationen_US
dc.typeThesisen_US


Files in this item

Thumbnail

Items in Knowledge Bank are protected by copyright, with all rights reserved, unless otherwise indicated.

This item appears in the following Collection(s)

Show simple item record