Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Chunwan Wei"'
Publikováno v:
Crystals, Vol 11, Iss 8, p 962 (2021)
Barite is an abundant sulfate mineral in nature. Especially, the variety of morphologies of barite is often driven by the mixing of Ba-bearing hydrothermal fluid and sulfate-bearing seawater around hydrothermal chimneys. In order to better understand
Externí odkaz:
https://doaj.org/article/d375a42122424832834fdccbda81bb41
Publikováno v:
Geochimica et Cosmochimica Acta. 343:371-383
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::47865b45399ec9833e50fc93d60c0cbd
https://doi.org/10.1016/j.gca.2022.12.019
https://doi.org/10.1016/j.gca.2022.12.019
Autor:
Aiguo Shi, Cheng Xu, Anton R. Chakhmouradian, Martin P. Smith, Jindrich Kynicky, Chaoxi Fan, Chunwan Wei, Guangxi Kuang
Publikováno v:
American Mineralogist. 107:2261-2271
Weathering crusts after granites are the most important source of heavy rare-earth elements (HREE) worldwide. Although HREE in these deposits is known to be inherited from parental rocks, the origin of HREE enrichment and the reasons why it is rare o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a176e475e608fb2463e23e93864959c
https://doi.org/10.2138/am-2022-8309
https://doi.org/10.2138/am-2022-8309
Publikováno v:
Crystals
Volume 11
Issue 8
Crystals, Vol 11, Iss 962, p 962 (2021)
Volume 11
Issue 8
Crystals, Vol 11, Iss 962, p 962 (2021)
Barite is an abundant sulfate mineral in nature. Especially, the variety of morphologies of barite is often driven by the mixing of Ba-bearing hydrothermal fluid and sulfate-bearing seawater around hydrothermal chimneys. In order to better understand
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e57556cd67731f6046a550c3dc001f7
Publikováno v:
Precambrian Research. 366:106427
Granitoids are the dominant component of the continental crust and can be used as probes for crustal formation and evolution. The origin of granites, especially ambiguous granites with alkaline affinities emplaced in orogenic settings, however, remai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75c51307f6e2a817efa6b037546f0bb2
https://doi.org/10.1016/j.precamres.2021.106427
https://doi.org/10.1016/j.precamres.2021.106427
Autor:
Jindřich Kynický, Chunwan Wei, Miao Deng, Liang Zeng, Y. Li, Meng Feng, Wenlei Song, Cheng Xu
Publikováno v:
Precambrian Research. 302:298-311
The North China Craton (NCC) is one of the oldest cratons in the world that preserves the records of many important geological events in the early evolution of the Earth. However, the early Precambrian tectonic evolution history of the NCC is still c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e44a972a1081086b96793750200a2581
https://doi.org/10.1016/j.precamres.2017.10.015
https://doi.org/10.1016/j.precamres.2017.10.015
Publikováno v:
Precambrian Research. 337:105557
Syenites are commonly associated with alkaline silicate rocks and carbonatites. The origin of syenites, however, remains controversial. Here, we report an intrusive suite of carbonatite–clinopyroxenite–clinopyroxene syenite complexes and granites
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb5624044fd0bef2d0bfa5c1b19c2bb5
https://doi.org/10.1016/j.precamres.2019.105557
https://doi.org/10.1016/j.precamres.2019.105557
Autor:
Wenlei Song, Chunwan Wei, Jindrich Kynicky, Meng Feng, Martin Brtnicky, Wei Fu, Michaela Kotlanova, Martin Smith, Clinten Cox
Publikováno v:
Ore Geology Reviews. 117:103294
Carbonatites are abundant in the rare earth elements (REE), and they host the most important REE resources in the world. However, the mechanisms that concentrate these elements during carbonatitic magmatic processes are still poorly constrained. Here
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9bf5edf6023f516fb79b15d37acb3fa1
https://doi.org/10.1016/j.oregeorev.2019.103294
https://doi.org/10.1016/j.oregeorev.2019.103294
Autor:
Cheng Xu, Chunwan Wei, Qihai Shu, Kangjun Huang, Martin Smith, Li Zhou, Wenlei Song, Jindrich Kynicky
Publikováno v:
Scientific Reports
Carbonatites, usually occurring within intra-continental rift-related settings, have strong light rare earth element (LREE) enrichment; they rarely contain economic heavy REE (HREE). Here, we report the identification of Late Triassic HREE-Mo-rich ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b1ed47862f9a4f5ce9d249beb34eb831