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Title: Comparison of clumped isotope signatures of dolomite cements to fluid inclusion thermometry in the temperature range of 73–176 °C

Authors:
; ; ;
Publication Date:
Sponsoring Org.:
USDOE
OSTI Identifier:
1411454
Resource Type:
Journal Article: Publisher's Accepted Manuscript
Journal Name:
Geochimica et Cosmochimica Acta
Additional Journal Information:
Journal Volume: 199; Journal Issue: C; Related Information: CHORUS Timestamp: 2018-09-07 01:21:10; Journal ID: ISSN 0016-7037
Publisher:
Elsevier
Country of Publication:
United States
Language:
English

Citation Formats

Came, Rosemarie E., Azmy, Karem, Tripati, Aradhna, and Olanipekun, Babatunde-John. Comparison of clumped isotope signatures of dolomite cements to fluid inclusion thermometry in the temperature range of 73–176 °C. United States: N. p., 2017. Web. doi:10.1016/j.gca.2016.10.028.
Came, Rosemarie E., Azmy, Karem, Tripati, Aradhna, & Olanipekun, Babatunde-John. Comparison of clumped isotope signatures of dolomite cements to fluid inclusion thermometry in the temperature range of 73–176 °C. United States. doi:10.1016/j.gca.2016.10.028.
Came, Rosemarie E., Azmy, Karem, Tripati, Aradhna, and Olanipekun, Babatunde-John. Wed . "Comparison of clumped isotope signatures of dolomite cements to fluid inclusion thermometry in the temperature range of 73–176 °C". United States. doi:10.1016/j.gca.2016.10.028.
@article{osti_1411454,
title = {Comparison of clumped isotope signatures of dolomite cements to fluid inclusion thermometry in the temperature range of 73–176 °C},
author = {Came, Rosemarie E. and Azmy, Karem and Tripati, Aradhna and Olanipekun, Babatunde-John},
abstractNote = {},
doi = {10.1016/j.gca.2016.10.028},
journal = {Geochimica et Cosmochimica Acta},
number = C,
volume = 199,
place = {United States},
year = {Wed Feb 01 00:00:00 EST 2017},
month = {Wed Feb 01 00:00:00 EST 2017}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record at 10.1016/j.gca.2016.10.028

Citation Metrics:
Cited by: 4 works
Citation information provided by
Web of Science

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