Titlebook: Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China; Hao Zou,Shou-Ting Zhang,Zhan-Zhang Xu Book 2022 The Editor(s) (

Gullet

書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China影響因子(影響力)




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China影響因子(影響力)學(xué)科排名




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China網(wǎng)絡(luò)公開度




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China被引頻次




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China被引頻次學(xué)科排名




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China年度引用




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China年度引用學(xué)科排名




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China讀者反饋




書目名稱Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China讀者反饋學(xué)科排名

Phagocytes

inspiration

https://doi.org/10.1007/978-1-4020-6752-5 Niutitang Formation. Using the Sm-Nd isotopic age of fluorite, combined with the formation time of other deposits in the study area, it is concluded that the mineralization age of this mineralization belt is the late Yanshan period (104?±?11?Ma).

CURB

Isotope Geochemistry, Niutitang Formation. Using the Sm-Nd isotopic age of fluorite, combined with the formation time of other deposits in the study area, it is concluded that the mineralization age of this mineralization belt is the late Yanshan period (104?±?11?Ma).

吸引力

可行

AFFIX

合并

Book 2022on, concentration, enrichment, and evolution of ore-forming sources, exploring the formation mechanism of barite-fluorite deposits. Summarizing the mineralization regularity of the deposit in this area of China provides a new insight and basis forthe study of similar types of deposits in the world..

樹木心

Petrological Characteristics and Sedimentary Environment,stone and dolomite. In addition, the open platform environment of the carbonate platform in the Lower Ordovician Tongzi Formation, the Lower Ordovician Honghuayuan Formation belonged to the platform marginal environment, both of which are conducive to the enrichment of fluorite.

放牧

Introduction,terial sources, etc. Based on the above content, it is concluded that there are some problems in the barite-fluorite deposits in this area that need to be resolved. Then introduced the ideas used to solve these problems and the main research content.