Origin of dolomite in the Middle Ordovician peritidal platform carbonates in the northern Ordos Basin, western China

Autor:	Xiaoqi Ding, Qing-Yu Huang, Xiao-Liang Bai, Si-Yang Zhang, Shao-Nan Zhang
Rok vydání:	2016
Předmět:	Recrystallization (geology) Evaporite 020209 energy Dolomite Geochemistry Energy Engineering and Power Technology Mineralogy Geology 02 engineering and technology 010502 geochemistry & geophysics Geotechnical Engineering and Engineering Geology 01 natural sciences Sedimentary depositional environment Petrography Geophysics Fuel Technology Geochemistry and Petrology Stylolite 0202 electrical engineering electronic engineering information engineering Dolomitization Ordovician Economic Geology 0105 earth and related environmental sciences
Zdroj:	Petroleum Science. 13:434-449
ISSN:	1995-8226 1672-5107
DOI:	10.1007/s12182-016-0114-5
Popis:	The carbonates in the Middle Ordovician Ma 5 5 submember of the Majiagou Formation in the northern Ordos Basin are partially to completely dolomitized. Two types of replacive dolomite are distinguished: (1) type 1 dolomite, which is primarily characterized by microcrystalline (
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b3d8d78571224642e310961edc8f03c4 https://doi.org/10.1007/s12182-016-0114-5 Zobrazit plný text záznamu Plný text ve formátu PDF