Matches in SemOpenAlex for { <https://semopenalex.org/work/W4295122731> ?p ?o ?g. }
- W4295122731 endingPage "8984" @default.
- W4295122731 startingPage "8984" @default.
- W4295122731 abstract "Typical stratiform-like cassiterite–sulfide orebodies formed at 160–150 Ma cut by a steep hydrothermal vein-type orebody were discovered in the Xianghualing tin–polymetallic orefield, which implied a new phase of magmatism and mineralization later than the Late Jurassic stage. Hence, a systematic study of the characteristics and genesis of the concealed Laohuya granite, including U–Pb age, trace elements, Lu–Hf isotopes of zircons, and whole-rock major- and trace-elements, is examined in this paper. The zircon U–Pb dating yielded a Concordia age of 87.75 ± 1 Ma, confirming the existence of Late Cretaceous magmatism in the Xianghualing tin–polymetallic orefield. The Laohuya granite is classified as syenogranite and belongs to the peraluminous, high K calc-alkaline series. It is a highly evolved A2-type granite with εHf(t) values ranging from −14.97 to −7.59 and two-stage model ages (TDM2) ranging from 2939 to 2280 Ma. Combining chronology, petrochemistry, isotopic geochemistry, and previous tectonic studies, we believe that the Laohuya granite originated from the partial melting of a reworked ancient crust composed of TTGs, and its weathered sediments formed in subduction or collision zones at 2.5 Ga, controlled by the reactivation of the Chenzhou–Linwu deep fault in the extensional setting of South China during the Late Cretaceous." @default.
- W4295122731 created "2022-09-11" @default.
- W4295122731 creator A5009739992 @default.
- W4295122731 creator A5036455884 @default.
- W4295122731 creator A5050018758 @default.
- W4295122731 creator A5053709720 @default.
- W4295122731 creator A5062284542 @default.
- W4295122731 creator A5062595578 @default.
- W4295122731 creator A5083862643 @default.
- W4295122731 date "2022-09-07" @default.
- W4295122731 modified "2023-10-01" @default.
- W4295122731 title "Genesis and Significance of Late Cretaceous Granitic Magmatism in Xianghualing Tin–Polymetallic Orefield, Nanling Region, South China" @default.
- W4295122731 cites W1158726619 @default.
- W4295122731 cites W1541910269 @default.
- W4295122731 cites W1968583876 @default.
- W4295122731 cites W1970595625 @default.
- W4295122731 cites W1972544946 @default.
- W4295122731 cites W1974238090 @default.
- W4295122731 cites W1974499954 @default.
- W4295122731 cites W1977650828 @default.
- W4295122731 cites W1978561672 @default.
- W4295122731 cites W1987844446 @default.
- W4295122731 cites W1999166202 @default.
- W4295122731 cites W1999609683 @default.
- W4295122731 cites W1999708461 @default.
- W4295122731 cites W2006115440 @default.
- W4295122731 cites W2010623866 @default.
- W4295122731 cites W2017448452 @default.
- W4295122731 cites W2019409833 @default.
- W4295122731 cites W2024331643 @default.
- W4295122731 cites W2029597154 @default.
- W4295122731 cites W2034079431 @default.
- W4295122731 cites W2036443034 @default.
- W4295122731 cites W2037913789 @default.
- W4295122731 cites W2039226804 @default.
- W4295122731 cites W2042803182 @default.
- W4295122731 cites W2042991064 @default.
- W4295122731 cites W2051805987 @default.
- W4295122731 cites W2060811640 @default.
- W4295122731 cites W2066007974 @default.
- W4295122731 cites W2071103381 @default.
- W4295122731 cites W2072189126 @default.
- W4295122731 cites W2072620570 @default.
- W4295122731 cites W2074233105 @default.
- W4295122731 cites W2076830276 @default.
- W4295122731 cites W2076922633 @default.
- W4295122731 cites W2078105240 @default.
- W4295122731 cites W2087616277 @default.
- W4295122731 cites W2108971421 @default.
- W4295122731 cites W2112141276 @default.
- W4295122731 cites W2126884842 @default.
- W4295122731 cites W2138522501 @default.
- W4295122731 cites W2140093647 @default.
- W4295122731 cites W2148200895 @default.
- W4295122731 cites W2155803469 @default.
- W4295122731 cites W2192105522 @default.
- W4295122731 cites W2325858089 @default.
- W4295122731 cites W2338678163 @default.
- W4295122731 cites W2523649812 @default.
- W4295122731 cites W2594092089 @default.
- W4295122731 cites W2623351969 @default.
- W4295122731 cites W2771382009 @default.
- W4295122731 cites W2790215448 @default.
- W4295122731 cites W2796600848 @default.
- W4295122731 cites W2801981759 @default.
- W4295122731 cites W2886103464 @default.
- W4295122731 cites W2998878292 @default.
- W4295122731 cites W3002698227 @default.
- W4295122731 cites W3006721897 @default.
- W4295122731 cites W3044893766 @default.
- W4295122731 cites W3084286412 @default.
- W4295122731 cites W3092606981 @default.
- W4295122731 cites W3127885627 @default.
- W4295122731 cites W3146373286 @default.
- W4295122731 cites W3152204540 @default.
- W4295122731 cites W4241232322 @default.
- W4295122731 cites W4281630721 @default.
- W4295122731 cites W4285676292 @default.
- W4295122731 doi "https://doi.org/10.3390/app12188984" @default.
- W4295122731 hasPublicationYear "2022" @default.
- W4295122731 type Work @default.
- W4295122731 citedByCount "1" @default.
- W4295122731 countsByYear W42951227312022 @default.
- W4295122731 crossrefType "journal-article" @default.
- W4295122731 hasAuthorship W4295122731A5009739992 @default.
- W4295122731 hasAuthorship W4295122731A5036455884 @default.
- W4295122731 hasAuthorship W4295122731A5050018758 @default.
- W4295122731 hasAuthorship W4295122731A5053709720 @default.
- W4295122731 hasAuthorship W4295122731A5062284542 @default.
- W4295122731 hasAuthorship W4295122731A5062595578 @default.
- W4295122731 hasAuthorship W4295122731A5083862643 @default.
- W4295122731 hasBestOaLocation W42951227311 @default.
- W4295122731 hasConcept C111696902 @default.
- W4295122731 hasConcept C119127063 @default.
- W4295122731 hasConcept C12294951 @default.
- W4295122731 hasConcept C127313418 @default.
- W4295122731 hasConcept C151730666 @default.
- W4295122731 hasConcept C156622251 @default.