Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024449999> ?p ?o ?g. }
- W2024449999 endingPage "130" @default.
- W2024449999 startingPage "110" @default.
- W2024449999 abstract "Abstract The Quanji Massif is a cratonic fragment located on the northeastern margin of the Qinghai-Tibetan Plateau in western Qinghai Province, northwest China ( Fig. 1 ). This massif consists of pre-Neoproterozoic crystalline basement unconformably overlain by mid- to late-Neoproterozoic and Cambrian strata. The basement is dominantly made up of the Delingha complex and the supracrustal Dakendaban Group. The Delingha complex is made up of 2.24–2.39 Ga granitic gneisses with enclaves of dominant amphibolite and minor felsic gneisses as well as granulites. The supracrustal Dakendaban group is in tectonic contact with the Delingha Complex, and can be divided into the lower and upper Dakendaban sub-Groups. Data from detrital zircons show that the protolith rocks of these two sub-groups were deposited after ∼2.32 Ga, and ∼2.11 Ga, respectively. The detrital zircon age and Hf isotopic data and geological correlations suggest that the Quanji Massif was possibly fragmented from the Tarim Craton, and the Delingha complex was probably uplifted to become the major sedimentary source for the upper Dakendaban sub-group at ∼2.11 Ga. Our zircon Hf-isotope compositions demonstrate important crustal growth at 2.6–2.7 Ga and ∼2.5 Ga. Together with the important magmatic activity at ∼2.2–2.4 Ga and geological data, our results seem to suggest that the Tarim Craton was part of the North China Craton in its early evolutionary history but rifted away and joined the Yangtze Craton prior to the Neoproterozoic." @default.
- W2024449999 created "2016-06-24" @default.
- W2024449999 creator A5022310530 @default.
- W2024449999 creator A5046468748 @default.
- W2024449999 creator A5068285146 @default.
- W2024449999 creator A5074051679 @default.
- W2024449999 creator A5077567100 @default.
- W2024449999 date "2012-08-01" @default.
- W2024449999 modified "2023-10-15" @default.
- W2024449999 title "U–Pb and Hf isotopic compositions of detrital zircons from the paragneisses of the Quanji Massif, NW China: Implications for its early tectonic evolutionary history" @default.
- W2024449999 cites W1967087709 @default.
- W2024449999 cites W1967525372 @default.
- W2024449999 cites W1968306266 @default.
- W2024449999 cites W1971816008 @default.
- W2024449999 cites W1972079338 @default.
- W2024449999 cites W1974236193 @default.
- W2024449999 cites W1977431633 @default.
- W2024449999 cites W1977930002 @default.
- W2024449999 cites W1977938914 @default.
- W2024449999 cites W1979854640 @default.
- W2024449999 cites W1982272146 @default.
- W2024449999 cites W1982274555 @default.
- W2024449999 cites W1985854661 @default.
- W2024449999 cites W1987737497 @default.
- W2024449999 cites W1988167699 @default.
- W2024449999 cites W1988392086 @default.
- W2024449999 cites W1989090951 @default.
- W2024449999 cites W1990277683 @default.
- W2024449999 cites W1992177674 @default.
- W2024449999 cites W1992214963 @default.
- W2024449999 cites W1993638742 @default.
- W2024449999 cites W2001772043 @default.
- W2024449999 cites W2002955926 @default.
- W2024449999 cites W2004433109 @default.
- W2024449999 cites W2005030647 @default.
- W2024449999 cites W2005520120 @default.
- W2024449999 cites W2005851587 @default.
- W2024449999 cites W2008479856 @default.
- W2024449999 cites W2009127786 @default.
- W2024449999 cites W2010194005 @default.
- W2024449999 cites W2013431530 @default.
- W2024449999 cites W2016069722 @default.
- W2024449999 cites W2016245690 @default.
- W2024449999 cites W2016511472 @default.
- W2024449999 cites W2018209057 @default.
- W2024449999 cites W2020973699 @default.
- W2024449999 cites W2022859730 @default.
- W2024449999 cites W2023745225 @default.
- W2024449999 cites W2027170597 @default.
- W2024449999 cites W2028642961 @default.
- W2024449999 cites W2030128782 @default.
- W2024449999 cites W2031301607 @default.
- W2024449999 cites W2031317963 @default.
- W2024449999 cites W2031902554 @default.
- W2024449999 cites W2033354344 @default.
- W2024449999 cites W2035970163 @default.
- W2024449999 cites W2039072788 @default.
- W2024449999 cites W2039145047 @default.
- W2024449999 cites W2039872199 @default.
- W2024449999 cites W2043003723 @default.
- W2024449999 cites W2043493161 @default.
- W2024449999 cites W2044175358 @default.
- W2024449999 cites W2050582708 @default.
- W2024449999 cites W2051273227 @default.
- W2024449999 cites W2052028650 @default.
- W2024449999 cites W2057837508 @default.
- W2024449999 cites W2060244969 @default.
- W2024449999 cites W2061359484 @default.
- W2024449999 cites W2063006645 @default.
- W2024449999 cites W2063015334 @default.
- W2024449999 cites W2063754919 @default.
- W2024449999 cites W2063969703 @default.
- W2024449999 cites W2065463075 @default.
- W2024449999 cites W2073326270 @default.
- W2024449999 cites W2074167122 @default.
- W2024449999 cites W2074503780 @default.
- W2024449999 cites W2077112971 @default.
- W2024449999 cites W2077868949 @default.
- W2024449999 cites W2080325016 @default.
- W2024449999 cites W2082232276 @default.
- W2024449999 cites W2088105278 @default.
- W2024449999 cites W2088724130 @default.
- W2024449999 cites W2089954248 @default.
- W2024449999 cites W2090206242 @default.
- W2024449999 cites W2092963142 @default.
- W2024449999 cites W2094472503 @default.
- W2024449999 cites W2099996347 @default.
- W2024449999 cites W2102249420 @default.
- W2024449999 cites W2106566774 @default.
- W2024449999 cites W2118521832 @default.
- W2024449999 cites W2133042542 @default.
- W2024449999 cites W2138522501 @default.
- W2024449999 cites W2145087726 @default.
- W2024449999 cites W2147173695 @default.
- W2024449999 cites W2161238196 @default.
- W2024449999 cites W2168661179 @default.
- W2024449999 cites W2260902065 @default.
- W2024449999 cites W2403988321 @default.