Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Panlao Zhao"'
Publikováno v:
Geochimica et Cosmochimica Acta. 339:115-126
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f1643cab2f08291ff3b005f3de58f2e
https://doi.org/10.1016/j.gca.2022.10.020
https://doi.org/10.1016/j.gca.2022.10.020
Publikováno v:
Geology. 50:121-125
Most tungsten (W) and tin (Sn) deposits are associated with highly evolved granites derived from the anatexis of metasedimentary rocks. They are commonly separated in both space and time, and in the rare cases where the W and Sn mineralization are pa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a14deabcb9d87c7b3a503f13a293718
https://doi.org/10.1130/g49248.1
https://doi.org/10.1130/g49248.1
Magmatic-hydrothermal tin deposits form in response to efficient tin extraction upon magma degassing
Publikováno v:
Geochimica et Cosmochimica Acta. 316:331-346
Most of the global Sn resources are from granite-related ore deposits, which form in response to cassiterite precipitation from hydrothermal fluids. However, the physical and chemical controls on the efficiency of Sn extraction from upper crustal plu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b259e2bd47719eca05c6aa4626e51f46
https://doi.org/10.1016/j.gca.2021.09.011
https://doi.org/10.1016/j.gca.2021.09.011
Autor:
Shunda Yuan, Panlao Zhao
Partial melting and fractional crystallization modeling method, and explanation of supplemental figures.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::55901f19613b071863b40f44c537dbcc
https://doi.org/10.1130/geol.s.16674217
https://doi.org/10.1130/geol.s.16674217
Publikováno v:
Economic Geology. 113:1193-1208
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be3f98b42c45a62912634a258f3e974a
https://doi.org/10.5382/econgeo.2018.4587
https://doi.org/10.5382/econgeo.2018.4587
Publikováno v:
Ore Geology Reviews. 95:1140-1160
The world-class Dongpo orefield, located in the Nanling Range, South China, is famous for its large-scale accumulation of W–Sn–Mo–Bi–Pb–Zn–Ag deposits, which includes the giant Shizhuyuan W-Sn-Mo-Bi, Jinchuantang Sn-Bi, Yejiwei Sn-Cu and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea2293636d0e58b1f2dcac3c024a9e21
https://doi.org/10.1016/j.oregeorev.2017.12.005
https://doi.org/10.1016/j.oregeorev.2017.12.005
Publikováno v:
Lithos. :519-534
The recently recognized Qinhang metallogenic belt (QHMB) is an economically important intracontinental Mesozoic porphyry-skarn Cu-polymetallic metallogenic belt in South China. However, the origin of the ore-bearing magma and the major factors contro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::969a1672e15a1af4b359689800ba5fc6
https://doi.org/10.1016/j.lithos.2018.01.017
https://doi.org/10.1016/j.lithos.2018.01.017
Autor:
Chen Yan, Panlao Zhao, Haijie Zhao, Yabin Yuan, Shunda Yuan, Jingwen Mao, Yan Shuang, Dongliang Zhang, Jian-Tang Peng
Publikováno v:
Ore Geology Reviews. 93:200-210
Recently, the mineral potential of the area surrounding the granitic batholiths in the Nanling Range was highlighted by the discovery of a series of tungsten and tin deposits or occurrences hosted in or near the Penggongmiao and Guidong batholiths in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cba5344b2cd4ac2f160933ee4026d4a4
https://doi.org/10.1016/j.oregeorev.2017.12.025
https://doi.org/10.1016/j.oregeorev.2017.12.025
Autor:
Panlao Zhao, M. Santosh, Hanhan He, Qiuhong Xie, Liu Han, Zhaochong Zhang, Kaiyuan Wang, Ziliang Jin
Publikováno v:
Ore Geology Reviews. 138:104395
Skarn-type Fe deposits constitute a major source of iron in the world, and 57% of the high-grade iron ores in China are hosted by skarn deposits. Most researchers agree that skarn-type Fe deposits are genetically linked with the associated magmas and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af41d789309146e301eedb13ffaa772d
https://doi.org/10.1016/j.oregeorev.2021.104395
https://doi.org/10.1016/j.oregeorev.2021.104395
Publikováno v:
Lithos. :132-145
The Qin–Hang intra-continental porphyry–skarn Cu polymetallic belt (QHMB) is among the economically important metallogenic belts in South China. The significant differences in the size and metal assemblage of the Jurassic magmatic–hydrothermal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e96209169df4d27f2e3ddeaa02ce68ed
https://doi.org/10.1016/j.lithos.2017.08.016
https://doi.org/10.1016/j.lithos.2017.08.016