The Tongling ore district of the Middle-Lower Yangtze metallogenic belt is a famous Cu-Au-Fe-S polymetal region, and its tectonic deformation, magmatic evolution, and metallogenic processes have been studied for decades. In this article, we propose a comprehensive tectonic-magmatic-metallogenic model of the ore-forming mechanism …
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genesis of the Dongguashan copper (gold) ore deposit in the Tongling ore district, Eastern China Zhong-fa Liu... oregeorev.2018.05.019 OREGEO 2593 To appear in: ... learning methods: a case study from Tongling ore district, eastern China Tao Sun, Fei Chen, Lianxiang Zhong... oregeorev.2019.04.003 OREGEO 2891 To appear in: ...
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DOI: 10.1016/S1002-0721(06)60175-0 Corpus ID: 136443640; Rare Earth Element Geochemistry on Magmatic Rocks and Gold Deposits in Shizishan Ore-Field of Tongling, China @article{Xu2006RareEE, title={Rare Earth Element Geochemistry on Magmatic Rocks and Gold Deposits in Shizishan Ore-Field of Tongling, China}, author={Xiaochun Xu and Sanming Lu …
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The localization patterns and mechanisms of orebody formation are critical in understanding and exploring for mineral deposits. Skarn ore deposits are especially difficult to study because of their complex features. The Fenghuangshan ore field is a maturely explored skarn copper ore field with many underground workings that reveal the skarn orebodies and related geological context in …
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The Tongling ore district is one of the most economically important ore areas in the Middle–Lower Yangtze River Metallogenic Belt, eastern China. It contains hundreds of polymetallic copper–gold deposits and occurrences. Those deposits are mainly clustered (from west to east) within the Tongguanshan, Shizishan, Xinqiao, Fenghuangshan, and Shatanjiao …
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REE geochemical characteristics of the magmatic rocks and gold deposits in Shizishan ore-field of Tongling were studied. Three types of the magmatic rocks have almost the same chondrite-normalized ...
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The Dongguashan copper-(gold) deposit is located in the Eastern Tongling ore district of the Middle-Lower Yangtze River Valley Metallogenic Belt (MLYRB), Eastern China. The Cu-(Au) …
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The Cishan gold deposit is a newly discovered medium-scale independent skarn gold deposit located in the Tongling ore cluster area of the Middle-Lower Yangtze Metallogenic Belt, and the ore ...
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The Dongguashan copper (gold) deposit in Anhui Province is one of the largest copper (gold) deposits in the Tongling ore district, which is the most important region in the Middle–Lower Yangtze ...
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Recognizing the evolution of the stratabound polymetallic massive sulfide deposits in Tongling mineralization cluster, East China through colloform pyrite. Ore Geology Reviews, 104915. ... Pirajno, F., and Zengjie Zhang (2007): Geodynamic settings and tectonic model of skarn gold deposits in China: An overview. Ore Geology Reviews 31, 139-169 ...
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Studies of both field and ore microscopy indicate that the gold-bearing sulfide ore is major gold ore type in the Chaoshan gold deposit.Bismuth mineral,one of major gold-carrying minerals,has a typomorphic significant and an important clue for prospecting of Chaoshan deposit.Ore textures mainly include crystalline-granular and filling-metasomatic textures with various shapes.Ore …
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Dongguashan deposit is a large porphyry-skarn copper (gold) deposit in Tongling ore district. The Qingshanjiao intermediate acid intrusion of Yanshanian had a direct genetic relationship with ...
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Semantic Scholar extracted view of "Genesis of the Dongguashan skarn Cu-(Au) deposit in Tongling, Eastern China: Evidence from fluid inclusions and H-O-S-Pb isotopes" by Zhong-fa Liu et al. ... ( gold) deposit is located in the Tongling copper-gold ore district of the Middle-Lower Yangtze River metallogenic belt. It is one of the most important ...
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Shujiadian Mine, Xinqiao ore field, Tongling, Anhui, China : porphyry skarn deposit . Log In Register. ... ⓘ Gold. List of minerals for each chemical element. Other Regions, Features and …
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The Hehuashan Pb–Zn deposit is located in the Tongling ore district, Anhui province, East China, which is the first large Pb–Zn deposit hosted by the dolostone and limestone units of the Lower Triassic in the Tongling district in Middle–Lower Yangtze River Metallogenic Belt (MLYRMB) (Liu et al., 2017, 2018).
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The Huangshilao gold deposit (>13.5 t Au) is comprised of stratabound pyrite‐dominant massive sulfide ores, and is distinguished from the skarn Cu, Au, and Cu–Au deposits that are dominant in the Tongguanshan orefield, Tongling, east‐central China. The stratabound orebodies are situated along flexural slip faults along the unconformity between the Upper Devonian Wutong and the …
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Yaojialing zinc-gold polymetallic ore deposit, located in the transitional area between the Tongling uplift region and the Fanchang fault basin, is a recently-discovered large zinc-gold deposit in ...
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The Cishan gold deposit is a newly discovered medium-scale independent skarn gold deposit located in the Tongling ore cluster area of the Middle-Lower Yangtze Metallogenic Belt, and the ore ...
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The Shizishan ore field is the largest and most intensively studied of the five ore fields that form the Tongling mining district. It is about 7 km to the east of Tongling, located at the intersection of the E–W-trending Tongling–Shatanjiao tectonic–magmatic belt and the Qingshan anticline of the NE–SW-trending Shun'an synclinorium.Within the Shizishan ore field, …
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The Tongling ore-cluster region is an important ore district of the famous Lower Yangtze River Metallogenic Belt (LYRB) in central eastern China, representing typical skarn deposits in China ...
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DOI: 10.1016/j.oregeorev.2024.105955 Corpus ID: 267753419; Gold mineralisation by pyrite recrystallisation and arsenopyrite sequestration in the Jiaochong Au deposit, Tongling ore district, eastern China: Implications for the formation of stratabound ore deposits
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The Shizishan copper (gold) ore-field is the largest in the Tongling ore district. The field is characterized by complex metallogenic processes as indicated by its dominantly skarn-type and stratabound skarn-type deposits. These deposits are rich in fluid inclusions with homogenization temperatures that range from 140 to 570°C and salinities that range from 1.07 to 60.72 wt% …
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Jinkouling Mine (Jingkouling Mine), Tongguanshan ore field, Tongling, Anhui, China : Skarn-type copper-gold deposit. Metal resource: 55,694 t Cu (@0.97%)
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The Middle–Lower Yangtze River Valley Metallogenetic Belt (MLYRB), a large and economically valuable porphyry–skarn–stratabound Cu–Au ore belt in China (Mao et al., 2011), has a total reserve of > 600 t of gold (Zhao et al., 1999).The orebodies in this belt are stratabound and lie parallel to the bedding of Upper Devonian to Lower Triassic carbonate strata (Mao et …
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1 Introduction. The Huangshilao stratabound gold deposit is located in the Tongling ore district in the Middle-Lower Yangtze River metallogenic belt, east-central China (Fig. 1).The belt, extending from Wuhan in the eastern Hubei Province in the west to Zhenjiang in the southern Jiangsu Province in the east, is a well-known Cu–Mo–Au–Fe polymetallic belt and contains …
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Secondly, the gold ore is rich in bismuth minerals, most of which are major gold-bearing minerals. Thirdly, there is a prominent positive correlation of Au with Bi in the gold ore. ... Discussion on the metallogenic depth of skarn type gold deposits in Tongling area, Anhui province. Geotectonica et Metallogenia 4:397–403. ... Several gold ...
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The Fenghuangshan copper–gold deposit, located in the Tongling ore cluster field along the Lower Yangtze metallogenic belt (LYRB) in eastern China, mainly consist of skarn ores hosted in ...
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Shizishan ore-field is a nonferrous and noble metal ore-field which is most rich in copper and gold.There are many types of fluid inclusions in minerals of the deposits.The homogeneous temperatures and the salinities of the fluid inclusions in main mineralization stages have wide ranges,while the different types of the fluid inclusions existed together and their homogeneous …
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The Shizishan copper (gold) ore-field is the largest in the Tongling ore district. The field is characterized by complex metallogenic processes as indicated by its dominantly skarn-type and stratabound skarn-type deposits. These deposits are rich in fluid inclusions with homogenization temperatures that ran ge from 140
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