Oxygen Isotope Microanalysis By Secondary Ion Mass Spectrometry Suggests Continuous 300-million-year History of Calcite Cementation and Dolomitization in the Devonian Bakken Formation-Reference-Cited by-同舟云学术

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Oxygen Isotope Microanalysis By Secondary Ion Mass Spectrometry Suggests Continuous 300-million-year History of Calcite Cementation and Dolomitization in the Devonian Bakken Formation

Published:2018-01-23 Issue:1 Volume:88 Page:91-104
ISSN:1527-1404
Container-title:Journal of Sedimentary Research
language:en
Short-container-title:

Author:

Brodie Mark W.,Aplin Andrew C.,Hart Bruce,Orland Ian J.,Valley John W.,Boyce Adrian J.

Publisher

Society for Sedimentary Geology

Subject

Geology

Link

http://pubs.geoscienceworld.org/jsedres/sepm/jsedres/article-pdf/88/1/91/4034004/i1527-1404-88-1-91.pdf

Cited by 12 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Carbon and oxygen isotope microanalysis of calcite in the Permian Kupferschiefer system, Saale subbasin, eastern Germany;Chemical Geology;2023-12

2. Geochemistry Characteristics of Source Rocks and Oil–Source Correlation in the Gaosheng Area of the Western Depression in the Liaohe Basin, Northeastern China;Energy & Fuels;2023-11-20

3. Modeling the maturation history of the stacked petroleum systems of the Williston Basin, USA;Marine and Petroleum Geology;2023-09

4. The Eocene-Oligocene climate transition in the Alpine foreland basin: Paleoenvironmental change recorded in submarine fans;Palaeogeography, Palaeoclimatology, Palaeoecology;2022-08

5. Chapter 10: Origin of Cements and Replacements;Sandstone Petrography, Petrology, and Modeling;2022-05-23

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