FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000634597> ?p ?o ?g. }

• W2000634597 endingPage "351" @default.
• W2000634597 startingPage "327" @default.
• W2000634597 abstract "In China, sediment-hosted Pb―Zn deposits represent a significant type of base-metal deposits are major sources of Pb and Zn and significant sources of Ag and Ge. In this paper, we focus discussion on MVT (Mississippi Valley type), SEDEX (sedimentary exhalative) and Jinding-type deposits because they constitute the major subtypes of sediment-hosted Pb―Zn deposits in China. For these deposits, which occur in a wide variety of carbonate and siliciclastic rocks having no obvious genetic association with igneous activity, we present an overview and re-evaluation with regard to: (1) nature, diversity, and geological settings, (2) spatio-temporal distributions, (3) structural controls on mineralization, (4) metallogenic process, and (5) C, O, S and Pb isotope geochemistry. Several of these deposits with known reserves are concentrated in eight main metallogenic belts. Available data from these deposits in China show the highest combined Zn and Pb reserves exist in the Qinling Mountains metallogenic belt, followed by the northern margin of the North China Craton (NCC), the Sanjiang fold belt, the Upper Yangtze River belt, the South China fold system, the Tianshan–Beishan Mountains belt, the Lower Yangtze River belt, and the Qilian Mountains belt. In these belts, the sediment-hosted Pb―Zn deposits have formed in a variety of tectonic settings representing a range of processes that have occurred within two billion years of earth history, but large-scale mineralizations have occurred notably in the Proterozoic, Late Paleozoic and Cenozoic. The Proterozoic era was important for the formation of SEDEX Pb―Zn deposits such as those in the interior and along the edges of the NCC and Yangtze Craton. The Guanmenshan is the only known MVT deposit formed within an intra-continental basin in the Proterozoic era. The Late Paleozoic was a productive period for MVT Pb―Zn deposits in China; in particular, there were significant MVT mineralizations during Devonian to Permian as a result of the amalgamation of the NCC and the South China Craton. The Cenozoic was a significant metallogenic era in China. For example, in the Sanjiang area during the Cenozoic, the Lanping Basin has evolved from a passive margin to open ocean basin and then has experienced ocean basin closure followed by the India–Asia collision and related tectonic activities including thrusting, and formation of strike–slip extensional basins, in which the Jinding-type deposits developed." @default.
• W2000634597 created "2016-06-24" @default.
• W2000634597 creator A5006377711 @default.
• W2000634597 creator A5007016189 @default.
• W2000634597 creator A5011053475 @default.
• W2000634597 creator A5056054711 @default.
• W2000634597 date "2014-01-01" @default.
• W2000634597 modified "2023-10-02" @default.
• W2000634597 title "Nature, diversity and temporal–spatial distributions of sediment-hosted Pb―Zn deposits in China" @default.
• W2000634597 cites W134687651 @default.
• W2000634597 cites W1678564827 @default.
• W2000634597 cites W1846261613 @default.
• W2000634597 cites W1964830566 @default.
• W2000634597 cites W1965979466 @default.
• W2000634597 cites W1966327538 @default.
• W2000634597 cites W1969185593 @default.
• W2000634597 cites W1970621049 @default.
• W2000634597 cites W1971984857 @default.
• W2000634597 cites W1980577867 @default.
• W2000634597 cites W1988966951 @default.
• W2000634597 cites W1996473326 @default.
• W2000634597 cites W2001290672 @default.
• W2000634597 cites W2002443467 @default.
• W2000634597 cites W2002557472 @default.
• W2000634597 cites W2003454252 @default.
• W2000634597 cites W2008874442 @default.
• W2000634597 cites W2016212752 @default.
• W2000634597 cites W2019151034 @default.
• W2000634597 cites W2023424842 @default.
• W2000634597 cites W2025880666 @default.
• W2000634597 cites W2028494985 @default.
• W2000634597 cites W2036924021 @default.
• W2000634597 cites W2040358312 @default.
• W2000634597 cites W2042354793 @default.
• W2000634597 cites W2045368211 @default.
• W2000634597 cites W2052892511 @default.
• W2000634597 cites W2061145580 @default.
• W2000634597 cites W2072539038 @default.
• W2000634597 cites W2078703472 @default.
• W2000634597 cites W2087684271 @default.
• W2000634597 cites W2092966734 @default.
• W2000634597 cites W2093503795 @default.
• W2000634597 cites W2094982079 @default.
• W2000634597 cites W2095563214 @default.
• W2000634597 cites W2098887892 @default.
• W2000634597 cites W2110767358 @default.
• W2000634597 cites W2113536738 @default.
• W2000634597 cites W2118655701 @default.
• W2000634597 cites W2131658178 @default.
• W2000634597 cites W2132454796 @default.
• W2000634597 cites W2134012677 @default.
• W2000634597 cites W2139660398 @default.
• W2000634597 cites W2143703034 @default.
• W2000634597 cites W2144662784 @default.
• W2000634597 cites W2148731911 @default.
• W2000634597 cites W2153825933 @default.
• W2000634597 cites W2158815859 @default.
• W2000634597 cites W2159792889 @default.
• W2000634597 cites W2164834123 @default.
• W2000634597 cites W2348737198 @default.
• W2000634597 cites W2600948397 @default.
• W2000634597 cites W2973238850 @default.
• W2000634597 cites W4237813084 @default.
• W2000634597 doi "https://doi.org/10.1016/j.oregeorev.2013.06.004" @default.
• W2000634597 hasPublicationYear "2014" @default.
• W2000634597 type Work @default.
• W2000634597 sameAs 2000634597 @default.
• W2000634597 citedByCount "100" @default.
• W2000634597 countsByYear W20006345972014 @default.
• W2000634597 countsByYear W20006345972015 @default.
• W2000634597 countsByYear W20006345972016 @default.
• W2000634597 countsByYear W20006345972017 @default.
• W2000634597 countsByYear W20006345972018 @default.
• W2000634597 countsByYear W20006345972019 @default.
• W2000634597 countsByYear W20006345972020 @default.
• W2000634597 countsByYear W20006345972021 @default.
• W2000634597 countsByYear W20006345972022 @default.
• W2000634597 countsByYear W20006345972023 @default.
• W2000634597 crossrefType "journal-article" @default.
• W2000634597 hasAuthorship W2000634597A5006377711 @default.
• W2000634597 hasAuthorship W2000634597A5007016189 @default.
• W2000634597 hasAuthorship W2000634597A5011053475 @default.
• W2000634597 hasAuthorship W2000634597A5056054711 @default.
• W2000634597 hasConcept C109007969 @default.
• W2000634597 hasConcept C114793014 @default.
• W2000634597 hasConcept C126753816 @default.
• W2000634597 hasConcept C127313418 @default.
• W2000634597 hasConcept C13106087 @default.
• W2000634597 hasConcept C147717901 @default.
• W2000634597 hasConcept C151730666 @default.
• W2000634597 hasConcept C17409809 @default.
• W2000634597 hasConcept C2776152364 @default.
• W2000634597 hasConcept C2779870107 @default.
• W2000634597 hasConcept C42787717 @default.
• W2000634597 hasConcept C6494504 @default.
• W2000634597 hasConcept C7145564 @default.
• W2000634597 hasConcept C77928131 @default.
• W2000634597 hasConcept C93033518 @default.

• next