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pro vyhledávání: '"FANG Weixuan"'
Publikováno v:
In Applied Geochemistry October 2024 173
Publikováno v:
Dizhi lixue xuebao, Vol 30, Iss 1, Pp 88-106 (2024)
Objective In the matter of material architecture, the diagenetic-metallogenic system may be classified into lithofacies of root-feeders (metallogenic material feeders), lithofacies of structural channel (migration of diagenetic-metallogenic material)
Externí odkaz:
https://doaj.org/article/db416bf52f224074bad8418ed6616276
Autor:
FANG Weixuan
Publikováno v:
Dizhi lixue xuebao, Vol 28, Iss 1, Pp 1-21 (2022)
The coupling pattern between the deformation history of tectonic lithofacies and the sequence of ore (reservoir)-forming in the basin remain as an unsettled scientific issue, for (non-) metals, uranium, coal, oil and gas resources being hosted in the
Externí odkaz:
https://doaj.org/article/412f1603158047f8844db57e4070fd7b
Autor:
JIA Runxing, FANG Weixuan
Publikováno v:
Dizhi lixue xuebao, Vol 28, Iss 1, Pp 67-77 (2022)
The Gejiu tin deposit in Yunnan Province is a world-class super-large tin-polymetallic deposit, and the interbedded deposit (cassiterite-sulfide) is one of the important deposit types, but its genesis has been debated. The mineral fabric and geochemi
Externí odkaz:
https://doaj.org/article/483e302d52d24ea48c77261c89809c79
Publikováno v:
Dizhi lixue xuebao, Vol 28, Iss 1, Pp 101-112 (2022)
The Kangsu area is located in the basin-mountain coupling zone formed by the alluvial action of the West Kunlun Mountains and the Southwestern Tianshan Mountains. Its tectonic landforms show significant characteristics of mountain-plain distribution
Externí odkaz:
https://doaj.org/article/7abf99aa46234c739e307f9a1744cff2
Publikováno v:
Dizhi lixue xuebao, Vol 28, Iss 1, Pp 22-35 (2022)
Many medium to large magnetite-type IOCG deposits have been found in the Copiapo area of Chile, which is located in the north fragment of the Chilean iron belt on the east side of the coastal mountain belt. The formation of these deposits is closely
Externí odkaz:
https://doaj.org/article/9b501057794c466db95908d29446f42c
Akademický článek
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Akademický článek
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Publikováno v:
Dizhi lixue xuebao, Vol 27, Iss 6, Pp 1035-1050 (2021)
Jinzhong Basin is a Cenozoic intracontinental faulted sedimentary basin located in the middle of Fen-Wei graben system. Our study aims to identify the Quaternary sedimentary sequence and reveal the Quaternary sedimentary environmental evolution of th
Externí odkaz:
https://doaj.org/article/cbef5b8966184f7dbf6d0ad8aaebf510
Autor:
JIA Runxing, FANG Weixuan
Publikováno v:
Dizhi lixue xuebao, Vol 27, Iss 4, Pp 529-541 (2021)
The Wulagen pb-zn deposit and the Sareke copper deposit, two most representative strata-bound glutenite deposits in the Meso-Cenozoic Basins in Southwestern Tianshan, are the subjects of our study. The Wulagen pb-zn deposit occurred in the coarse san
Externí odkaz:
https://doaj.org/article/c080693de17d407599819095c384c4f8