標(biāo)題: Titlebook: Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China; Hao Zou,Shou-Ting Zhang,Zhan-Zhang Xu Book 2022 The Editor(s) ( [打印本頁] 作者: Gullet 時間: 2025-3-21 16:29
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
作者: Phagocytes 時間: 2025-3-21 22:29 作者: inspiration 時間: 2025-3-22 02:55
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).作者: CURB 時間: 2025-3-22 06:53
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).作者: 吸引力 時間: 2025-3-22 10:42 作者: 可行 時間: 2025-3-22 16:04 作者: AFFIX 時間: 2025-3-22 19:17 作者: 合并 時間: 2025-3-22 22:37
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..作者: 樹木心 時間: 2025-3-23 01:27
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.作者: 放牧 時間: 2025-3-23 09:22
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.作者: 空氣 時間: 2025-3-23 10:36
https://doi.org/10.1007/978-981-16-7562-1Barite-fluorite deposits; Source of ore-forming material and fluid; Mineralization regularity; Isotope 作者: APO 時間: 2025-3-23 17:53 作者: 歌劇等 時間: 2025-3-23 18:13 作者: 撕裂皮肉 時間: 2025-3-23 23:32 作者: 變量 時間: 2025-3-24 03:41 作者: Resign 時間: 2025-3-24 09:23 作者: 方便 時間: 2025-3-24 11:51 作者: multiply 時間: 2025-3-24 15:48 作者: CLAY 時間: 2025-3-24 21:07
Zheng Wu,Christoph M. Schimmeleks include the shallow metamorphic clastic rocks of the Banxi Group, the Moraine conglomerate and conglomerate sandstone of the Ediacaran, and the Cambrian sandstone. The shale is mainly Cambrian black shale. Carbonate rocks include Cambrian-Ordovician limestone, bioclastic limestone, dolomitic lime作者: 暖昧關(guān)系 時間: 2025-3-25 00:14
https://doi.org/10.1007/978-1-4020-6752-5in southeast Sichuan are strictly controlled by the NE-trending fold fault zone. This fault zone is large in scale and the faults cut deep. Although it does not directly host minerals, the ore-forming wall rock alteration and barite-fluorite mineralization developed along the belt, and the NW-trendi作者: 五行打油詩 時間: 2025-3-25 04:43 作者: 混合 時間: 2025-3-25 11:11 作者: Overdose 時間: 2025-3-25 13:55 作者: ARCHE 時間: 2025-3-25 17:10
Zeng Yi,Dudley L. Poston,Danan Gution regularity. According to the .Sr/.Sr ratio, trace element and isotopic analysis results, the Cambrian–Ordovician carbonate strata could provide sufficient Ca for mineralization, and the source of Ca was most likely a multi-source. The Lower Cambrian Niutitang Formation (regional) in the study a作者: incontinence 時間: 2025-3-25 23:00 作者: Allure 時間: 2025-3-26 01:36
Element Geochemistry,stance was relatively long. The obtained Eu and Ce anomalies reflect that the ore was formed in an open system with high oxygen fugacity. According to the Tb/Ca-Tb/La and La/Yb-∑REE diagrams, the barite-fluorite deposits in the study area were of hydrothermal origin, magmatic fluids were not involve作者: jagged 時間: 2025-3-26 07:29 作者: 適宜 時間: 2025-3-26 10:46 作者: Dislocation 時間: 2025-3-26 13:57
1876-1682 on 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..978-981-16-7564-5978-981-16-7562-1Series ISSN 1876-1682 Series E-ISSN 1876-1690 作者: Perceive 時間: 2025-3-26 18:53
https://doi.org/10.1007/978-1-4020-6752-5adjacent areas occur in the Lower Ordovician Tongzi Formation and Fenxiang Formation. A small number of deposits of these formations and the Honghuayuan Formation occur in the first member of the Dawan Formation and the Baota Formation, with obvious characteristics of stratabound?deposits.作者: Ordeal 時間: 2025-3-26 21:40 作者: 無所不知 時間: 2025-3-27 04:55 作者: ureter 時間: 2025-3-27 08:36 作者: ungainly 時間: 2025-3-27 09:29
Barite-Fluorite Mineralization in Southeast Sichuan, Yangtze Block, China作者: BILL 時間: 2025-3-27 17:00
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.作者: 積云 時間: 2025-3-27 18:55
Geological Setting, the Sichuan Basin has experienced multiple tectonic movements (Caledonian, Hercynian, and Indosinian-Yanshan tectonic movements), and was especially influenced?by the Late Jurassic–Late Cretaceous Yanshan movement, during which the Neoproterozoic–Jurassic strata underwent strong folding and deforma作者: 狗舍 時間: 2025-3-27 22:58 作者: 集中營 時間: 2025-3-28 03:56 作者: 獨輪車 時間: 2025-3-28 08:50
Element Geochemistry,ns, it is clarified that the source of F and Ba is related to the Lower Cambrian Niutitang Formation. According to the REE distribution in fluorite and barite, δEu, δCe, and Y/Ho differentiation characteristics, it is inferred that the sources of the ore-forming materials in different mining areas o作者: Crumple 時間: 2025-3-28 12:19 作者: 朦朧 時間: 2025-3-28 14:58
Isotope Geochemistry,cteristics. Among them, H-O isotopes indicate that the sources of barite-fluorite ore-forming fluids in southeast Sichuan are multi-sources, derived from hot brine, formation water, and meteoric water. According to the S-Sr isotopes, it is found that the source of the ore-forming element Ca should b作者: 牢騷 時間: 2025-3-28 22:40
