Discuss on Genesis of Zhulinkou Lead-Zinc Deposit in Changyang County
Yang Wen-xue
Abstract
Yang Wen-xue
Abstract
The Zhulinkou lead-zinc deposit is discovered by Geological Survey Fund Project of Hubei Province from 2006 to 2008,As a typical stratabound hydrothermal deposit,it is found after deposits of Hejiaping and Wangjiawan in east segment of Changyang Anticline,several similarities between them in metallogenic geological background and ore-controlling structure conditions.The study on its genetic mechanism can guide the future prospecting in Changyang.Therefore,the Qiqiu lead-zinc deposit is analyzed from some aspects,including the geological structure,orebody geological characteristics,and rock geophysical features,for the purpose that discussing the metallogenic mechanism and environment to obtain its metallogenic rules finally,which is reference for further geological works.
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The Zhulinkou lead-zinc deposit is discovered by Geological Survey Fund Project of Hubei Province from 2006 to 2008,As a typical stratabound hydrothermal deposit,it is found after deposits of Hejiaping and Wangjiawan in east segment of Changyang Anticline,several similarities between them in metallogenic geological background and ore-controlling structure conditions.The study on its genetic mechanism can guide the future prospecting in Changyang.Therefore,the Qiqiu lead-zinc deposit is analyzed from some aspects,including the geological structure,orebody geological characteristics,and rock geophysical features,for the purpose that discussing the metallogenic mechanism and environment to obtain its metallogenic rules finally,which is reference for further geological works.
Key concepts: Geology, Anticline, Prospecting, Geochemistry, Lead (geology), Mining engineering, Hydrothermal circulation, Geomorphology