COMPARISON OF DIFFERENT MINERALIZATIONS IN MESOZOIC AND ITS SIGNIFICENCE IN JIAODONT REGION,SHANDONG PROVINCE
Guangmin Li
Abstract
Guangmin Li
Abstract
There are two mineralization stages , Yanshanian and Late-Yanshanian mineralization in Jiaodong region , Shandong Province . Yanshanian mineralization which formed quartz vein type ( Linglong tpye ) and altered rock type ( Jiaojia type ) gold deposits , has been studied for several years . It was related to the regional granitic magmatism which had been formed in compressive dynamic environment . Late-Yanshanian mineralization was related to Qingshanian middle-mafic magmatism in extension environment . Altered breccia type gold deposits , such as Pengjiakuang gold deposit , were formed in shallow depth ( 1 km~3 km ) . With the comparison of the ore-forming environments , geological characteristics and stable isotope of these two mineralization stages, this paper has proposed that Late-Yanshanian gold-multimetal mineralization is as important as Yanshanian gold mineralization in Jiaodong region . Studying the Late-Yanshanian mineralization in detail will be help to the enlargement of the gold reserves and the sustainable development of the gold industry in Shandong Province .
A significance statement is not available in the OpenAlex record.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
There are two mineralization stages , Yanshanian and Late-Yanshanian mineralization in Jiaodong region , Shandong Province . Yanshanian mineralization which formed quartz vein type ( Linglong tpye ) and altered rock type ( Jiaojia type ) gold deposits , has been studied for several years . It was related to the regional granitic magmatism which had been formed in compressive dynamic environment . Late-Yanshanian mineralization was related to Qingshanian middle-mafic magmatism in extension environment . Altered breccia type gold deposits , such as Pengjiakuang gold deposit , were formed in shallow depth ( 1 km~3 km ) . With the comparison of the ore-forming environments , geological characteristics and stable isotope of these two mineralization stages, this paper has proposed that Late-Yanshanian gold-multimetal mineralization is as important as Yanshanian gold mineralization in Jiaodong region . Studying the Late-Yanshanian mineralization in detail will be help to the enlargement of the gold reserves and the sustainable development of the gold industry in Shandong Province .
Key concepts: Mineralization (soil science), Magmatism, Geology, Geochemistry, Breccia, Gold ore, Mesozoic, Mafic