Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023160838> ?p ?o ?g. }
- W2023160838 endingPage "873" @default.
- W2023160838 startingPage "861" @default.
- W2023160838 abstract "The correlation between the North China Craton (NCC) and the Indian Shield (IND) has been a hot topic in recent years. On the basis of ore deposit databases, the NCC and IND have shown broad similarity in metallogenesis from the middle Archaean to the Mesoproterozoic. The two blocks both have three major metallogenic systems: (1) the Archaean BIF metallogenic system; (2) the Paleoproterozoic Cu-Pb-Zn metallogenic system; and (3) the Mesoproterozoic Fe-Pb-Zn system. In the north margin of the NCC and the west margin of the IND, the Archaean BIF-Au-Cu-Pb-Zn deposits had the same petrogenesis and host rocks, the Paleoproterozoic Cu-Pb-Zn deposits were controlled by active belts, and the Mesoproterozoic Fe-Pb-Zn deposits were mainly related to multi-stage rifting. Matching regional mineralization patterns and geological features has established the continental assembly referred to as “NCWI”, an acronym for the north margin of the NCC (NC) and the west margin of the IND (WI) during the middle Archaean to the Mesoproterozoic. In this assembly, the available geological and metallogenic data from the Eastern Block and active belts of NC fit those from the Dharwar craton and the Aravalli–Delhi–Vindhyan belt of WI, respectively. Moreover, the depositional model and environment of Paleoproterozoic metasedimentary manganese deposits in NCWI implied that the assembly may be located at low latitudes, where the conditions were favorable for dissolving ice and precipitating manganese deposits." @default.
- W2023160838 created "2016-06-24" @default.
- W2023160838 creator A5008493297 @default.
- W2023160838 creator A5013278632 @default.
- W2023160838 creator A5015180941 @default.
- W2023160838 creator A5029190681 @default.
- W2023160838 creator A5073861665 @default.
- W2023160838 creator A5088513591 @default.
- W2023160838 date "2015-11-01" @default.
- W2023160838 modified "2023-10-03" @default.
- W2023160838 title "Correlations between the North China Craton and the Indian Shield: Constraints from regional metallogeny" @default.
- W2023160838 cites W1653780642 @default.
- W2023160838 cites W1965625536 @default.
- W2023160838 cites W1968405128 @default.
- W2023160838 cites W1971787209 @default.
- W2023160838 cites W1971984857 @default.
- W2023160838 cites W1973511952 @default.
- W2023160838 cites W1974438203 @default.
- W2023160838 cites W1977431633 @default.
- W2023160838 cites W1980636746 @default.
- W2023160838 cites W1981165440 @default.
- W2023160838 cites W1982070838 @default.
- W2023160838 cites W1990642104 @default.
- W2023160838 cites W1996501609 @default.
- W2023160838 cites W2001251770 @default.
- W2023160838 cites W2002769103 @default.
- W2023160838 cites W2002953373 @default.
- W2023160838 cites W2004181256 @default.
- W2023160838 cites W2012878705 @default.
- W2023160838 cites W2015132357 @default.
- W2023160838 cites W2017568806 @default.
- W2023160838 cites W2017600130 @default.
- W2023160838 cites W2026652257 @default.
- W2023160838 cites W2032437752 @default.
- W2023160838 cites W2039587498 @default.
- W2023160838 cites W2043003723 @default.
- W2023160838 cites W2045711248 @default.
- W2023160838 cites W2045837211 @default.
- W2023160838 cites W2052964693 @default.
- W2023160838 cites W2061359484 @default.
- W2023160838 cites W2064362140 @default.
- W2023160838 cites W2065162710 @default.
- W2023160838 cites W2065463075 @default.
- W2023160838 cites W2068589066 @default.
- W2023160838 cites W2069762569 @default.
- W2023160838 cites W2071726845 @default.
- W2023160838 cites W2072681703 @default.
- W2023160838 cites W2074167122 @default.
- W2023160838 cites W2074436765 @default.
- W2023160838 cites W2077474983 @default.
- W2023160838 cites W2078458680 @default.
- W2023160838 cites W2079127500 @default.
- W2023160838 cites W2080423861 @default.
- W2023160838 cites W2082610919 @default.
- W2023160838 cites W2085954133 @default.
- W2023160838 cites W2092371852 @default.
- W2023160838 cites W2093411929 @default.
- W2023160838 cites W2093792770 @default.
- W2023160838 cites W2094472503 @default.
- W2023160838 cites W2114467958 @default.
- W2023160838 cites W2117935716 @default.
- W2023160838 cites W2119438065 @default.
- W2023160838 cites W2119523428 @default.
- W2023160838 cites W2129608368 @default.
- W2023160838 cites W2132909262 @default.
- W2023160838 cites W2136525356 @default.
- W2023160838 cites W2151039219 @default.
- W2023160838 cites W2165514703 @default.
- W2023160838 cites W2165712457 @default.
- W2023160838 cites W2165718688 @default.
- W2023160838 cites W2166465211 @default.
- W2023160838 cites W2170634279 @default.
- W2023160838 cites W3149707589 @default.
- W2023160838 doi "https://doi.org/10.1016/j.gsf.2015.03.004" @default.
- W2023160838 hasPublicationYear "2015" @default.
- W2023160838 type Work @default.
- W2023160838 sameAs 2023160838 @default.
- W2023160838 citedByCount "9" @default.
- W2023160838 countsByYear W20231608382017 @default.
- W2023160838 countsByYear W20231608382018 @default.
- W2023160838 countsByYear W20231608382019 @default.
- W2023160838 countsByYear W20231608382020 @default.
- W2023160838 countsByYear W20231608382021 @default.
- W2023160838 countsByYear W20231608382023 @default.
- W2023160838 crossrefType "journal-article" @default.
- W2023160838 hasAuthorship W2023160838A5008493297 @default.
- W2023160838 hasAuthorship W2023160838A5013278632 @default.
- W2023160838 hasAuthorship W2023160838A5015180941 @default.
- W2023160838 hasAuthorship W2023160838A5029190681 @default.
- W2023160838 hasAuthorship W2023160838A5073861665 @default.
- W2023160838 hasAuthorship W2023160838A5088513591 @default.
- W2023160838 hasBestOaLocation W20231608381 @default.
- W2023160838 hasConcept C119127063 @default.
- W2023160838 hasConcept C127313418 @default.
- W2023160838 hasConcept C147717901 @default.
- W2023160838 hasConcept C149347711 @default.
- W2023160838 hasConcept C151730666 @default.
- W2023160838 hasConcept C171991868 @default.