The moldic pore evolution of the Middle Ordovician sabkha dolostone in Ordos Basin, China: A study based on the petrographic and geochemical characteristics of pore fillings-Reference-Cited by-同舟云学术

The moldic pore evolution of the Middle Ordovician sabkha dolostone in Ordos Basin, China: A study based on the petrographic and geochemical characteristics of pore fillings

Published:2022-04-05 Issue:7 Volume:57 Page:2812-2827
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Luo Qingqing¹,Liu Bo²,Shi Kaibo¹,Luo Nina³,Yang Yunfei⁴,Shen Yingchu¹,Lu Feifan¹,Wei Liubin⁵,Wu Chun¹,Zhao Qing¹

Affiliation:

1. School of Earth and Space Sciences Peking University Beijing China

2. Institute of Oil and Gas Peking University Beijing China

3. Chongqing Gas Field of PetroChina Southwest Oil and Gas Field Company, PetroChina Chongqing China

4. The Third Oil Production Plant of Changqing Oilfield Company, PetroChina Yinchuan China

5. Exploration and Development Research Institute of Changqing Oilfield Company, PetroChina Xi'an China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4441

Reference75 articles.

1. Bao H. P.(2013).The characteristics and origin of the pore fillings of the weathering crust reservoirs at the top of Ordovician in central and eastern of the Ordos Basin. unpublished report.

2. Sedimentology study on sub‐member lithofacies paleogeography mapping and its petroleum exploration significance: Taking M5 member of Lower Ordovician Majiagou Formation in central‐eastern Ordos Basin for example;Bao H. P.;Acta Petrologica Sinica,2017

3. Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa

4. Comparing yttrium and rare earths in hydrothermal fluids from the Mid-Atlantic Ridge: implications for Y and REE behaviour during near-vent mixing and for the Y/Ho ratio of Proterozoic seawater

5. Rare earth element fractionation in metamorphogenic hydrothermal calcite, magnesite and siderite

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