Organic matter maturation in the contact aureole of an igneous sill as a tracer of hydrothermal convection-Reference-Cited by-同舟云学术

Organic matter maturation in the contact aureole of an igneous sill as a tracer of hydrothermal convection

Published:2015-06 Issue:6 Volume:120 Page:4102-4112
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Wang Dayong¹²,Manga Michael²

Affiliation:

1. Key Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, School of Energy and Power Engineering; Dalian University of Technology; Dalian China

2. Department of Earth and Planetary Science; University of California; Berkeley California USA

Funder

National Science Foundation of China

Fundamental Research Funds for the Central Universities

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015JB011877/fullpdf

Reference54 articles.

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3. A comparison of vitrinite reflectance measurements made on whole-rock and dispersed organic matter concentrate mounts;Barker;Org. Geochem.,1996

4. Fluid inclusion and vitrinite-reflectance geothermometry compared to heat-flow models of maximum paleotemperature next to dikes, western onshore Gippsland Basin, Australia;Barker;Int. J. Coal Geol.,1998

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