Petrographic and geochemical evidence of the diagenetic environment and fluid source of dolomitization of dolomite: a case study from the Ma55 to Ma51 submembers of the Ordovician Majiagou Formation, central Yishan Slope, Ordos Basin, China-Reference-Cited by-同舟云学术

Petrographic and geochemical evidence of the diagenetic environment and fluid source of dolomitization of dolomite: a case study from the Ma55 to Ma51 submembers of the Ordovician Majiagou Formation, central Yishan Slope, Ordos Basin, China

Published:2020-03-07 Issue:2 Volume:35 Page:
ISSN:0891-2556
Container-title:Carbonates and Evaporites
language:en
Short-container-title:Carbonates Evaporites

Author:

Li Baiqiang^ORCID,Wang Qicong,Zhang Xiaoli

Funder

the National “13th Five-Year” Plan for Science and Technology Major Project of China

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

http://link.springer.com/content/pdf/10.1007/s13146-020-00569-6.pdf

Reference100 articles.

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2. Alhelal AB, Whitaker FF, Spycher N, Xiao Y (2012) Modeling brine reflux using the Pitzer ion-interaction model in Toughreact. In: Proceedings of the TOUGH Symposium. Lawrence Berkeley Notional Laboratory, Berkeley, California, pp 841–847

3. Allan JR, Matthews RK (1982) Isotope signatures associated with early meteoric diagenesis. Sedimentology 29:797–817

4. Allan JR, Wiggins WD (1993) Dolomite reservoirs- geochemical techniques for evaluating origin and distribution. AAPG 36:129

5. Al-Aasm IS (2000) Chemical and isotopic constraints for recrystallization of sedimentary dolomites from the Western Canada Sedimentary Basin. Aquat Geochem 6:227–248

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