Title: On Genesis of the Middle Ordovician Patchy Dolomitite in the Northwest Ordos Basin
Abstract: The Middle Ordovician patchy dolomitite is widely exposed in the Northwest Ordos basin.Lithologic,mineralogical and geochemical studies indicate that the protolith was a crystal powder dolomite-aplite dolomite in the exogenetic stage with patchy aplite dolomite-crystal powder dolomite resulted from differential dolomitization in late diagenetic stage.
Publication Year: 2012
Publication Date: 2012-01-01
Language: en
Type: article
Access and Citation
AI Researcher Chatbot
Get quick answers to your questions about the article from our AI researcher chatbot