Zonation and genesis of the Red Mountain Red Bull skarns, Shangri-la Zhongdian, Yunnan Province, China, and the implications to exploration Supervisor Dr. Zhaoshan Chang July 2013 Background The Red Mountain Red Bull RMRB Cu skarn is located 40 km NE of the Shangri-la Zhongdian city in NW Yunnan Province, China.
Sulfide zonal texture and its geological significance of ores from the Hongshan copper deposit in Shangri-la, Yunnan Province, China. ACTA PETROLOGICA SINICA, 2013, 294 1203-1213. DOI
After the expert assessment, the new technology saved construction fund 5000000 yuan in 1991 prices, and Workers of Shanxi had reported thisSince 2006, the mining design of mine project and infrastructure investment technical and economic demonstration he has joined change the extension mining scheme design of Yunnan Shangri-La Hongshan ...
After making sure the ore preparability, Technology Support Department would contact with mineral dressing construction departments including geology, mining, ore dressing, ... change the extension mining scheme design of Yunnan Shangri-La Hongshan copper 5000td mining and dressing engineering design of Anhui Xiaoxian Flagpole building iron ...
Jan 28, 2021 Porphyry Cu-Au deposits PCDs have commonly multiphase porphyry intrusions, yet only one or a few of the intrusive phase isare ore-causative. Understanding the criteria to form ore-causative porphyry is important for both ore deposit research and PCD exploration. At the giant Pulang PCD in western Yunnan, there are three generations of porphyries, i.e., from oldest to youngest the
Emeishan Traps, Asia The Emeishan large igneous province is located in the provinces of Sichuan, Yunnan and Guizhou and extends into northern Vietnam.
Sep 20, 2017 Several Cretaceous Carlin-like or hydrothermal gold deposits along the Garze-Litang suture zone and Early Cretaceous hydrothermal copper mineralization along the southeastern margin of the Songpan-Garze fold belt were presumed to have a magmatic heat source. However, no actual coeval magmatic events nearby were discovered. Here, we report zircon SIMS U-Pb age, whole-rock
Mar 12, 2021 Art by Damien Marie AtHope. Hongshan culture 6,720-4,920 years ago. The Hongshan culture was a Neolithic culture in the Liao river basin in northeast China.Hongshan sites have been found in an area stretching from Inner Mongolia to Liaoning, and dated from about 4700 to 2900 BCE or 6,720-4,920 years ago. 63 of Hongshan sites had haplogroup N, which today is more common in
Adit WikipediaOverviewadit mining Britannica adit a horizontal or nearhorizontal passage driven from the Earths surface into the side of a ridge or mountain for the purpose of working,ampadit tunnel mining
Acanthite is the low-temperature modification of silver sulphide. All natural silver sulphide specimens at room temperature are acanthite. The structure of Argentite, the high-temperature cubic isometric form cannot be quenched.At atmospheric pressure, pure argentite is stable above 177 C and acanthite is stable below 177 C.
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Jun 11, 2020 1 Introduction The Hongshan deposit in Yunnan province is located in the Zhongdian area, which is commonly regarded as one of the most fertile regions for porphyry copper deposit in S.W. China Fig. 1 a because it hosts many large porphyryskarn deposits such as Pulang, Xuejiping, Hongshan, and Chundu Li et al., 2011a Yang et al., 2002 ...
Special Issue Meeting Abstracts The 14 th Quadrennial International Association on the Genesis of Ore Deposits Symposium. August 1922, 2014, Kunming, China
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Jan 05, 2014 The Hongniu-Hongshan porphyry and skarn copper deposit is located in the central part of the Zhongdian arc, Shangri-La County, Yunnan province, southwestern China, at 99 53E and 28 07N Fig. 1c, and at an elevation of 40604460 m.The deposit has two ore blocks termed the Hongshan and the Hongniu blocks.
The Pulang porphyry copper deposit is located 470 km NW to NNW of Kunming and 460 km SW of Chengdu on the Tibetan Plateau, in Shangri-La county, Yunnan province, southwestern China at an altitude of 3520 to 4570 m.a.s.l. It lies within the East Porphyry Belt of the southern subterrane of the Yidun Arc in the Yidun Terrane.
Nov 25, 2017 The Badi copper deposit is located in Shangjiang town, Shangri-La County, Yunnan Province. Tectonically, it belongs to the Sanjiang Block. Vaporliquid two-phase fluid inclusions, CO 2-bearing fluid inclusions, and daughter-bearing inclusions were identified in sulfide-rich quartz veins.Microthermometric and Raman spectroscopy studies revealed their types of ore-forming fluids
Jan 01, 2015 The Hongshan Cupolymetallic deposit is located about 30 km northeast of the city of Shangri-la Zhongdian Fig. 1b. The main exposed strata in the Hongshan ore district Fig. 2 comprise the second and third members of the Upper Triassic Qugasi Formation that are overlain unconformably or in fault contact with the second member of the ...
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After the expert assessment the new technology saved construction fund 5000000 yuan in 1991 prices and Workers of Shanxi had reported thisSince 2006 the mining design of mine project and infrastructure investment technical and economic demonstration he has joined change the extension mining scheme design of Yunnan Shangri-La Hongshan copper ...
Sep 25, 2018 1 State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 550081, Guiyang, China 2 University of Chinese Academy of Sciences, 100039, Beijing, China 3 Department of Earth and Atmospheric Sciences, Indiana University, Indiana 47405, Bloomington, U.S.A.
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Sulfide zonal texture and its geological significance of ores from the Hongshan copper deposit in Shangri-la, Yunnan Province, China B Zu, CJ Xue, XE Ya, QF Wang, HY Liang, Y Zhao, MT Liu Acta Petrologica Sinica 29 4, 1203-1213 , 2013
Sep 02, 2019 The LA was completed at an energy density of 10 Jcm 2 and a 10 Hz repetition rate with a spot size of 50 m. The Hf isotopic analysis was conducted on the UPb dating analysis position. The detailed operating conditions for the LA system and analytical methods have been described by Geng et al. Reference Geng, Li, Zhang, Zhou and Li 2011.
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