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• W2016690206 abstract "The Baoshan block is one of the important members in the southeastern margin of the Tibetan Plateau. Cambrian to Jurassic (meta-) sedimentary strata and their metamorphic counterparts were well preserved in the eastern part of the Baoshan block. Zircon U–Pb dating, trace elements, and Hf isotope data for both the Cambrian to Jurassic (meta-) sedimentary sequences and the Lincang granite were used to deduce the provenance of sediments and crustal affinity with eastern Gondwanaland. The Lincang granite outcropped in the Fengqing area is typical S-type, with crystallization age of ~ 230 Ma and narrow range of zircon εHf(t) values from − 15.5 to − 10. Detrital zircons from Paleozoic strata range in age from Archean to early Paleozoic, with age peaks at ~ 2.5, ~ 0.95, and ~ 0.6 Ga. Triassic age peak (~ 230 Ma) was also detected in the Jurassic strata. Detrital zircon εHf(t) values exhibit a wide range from negative to positive for each of the four major age groups, showing the host magma of zircons from these groups have diverse sources. The Baoshan block should be along the Indian margin as the Qiangtang, Tengchong and Simao–Indochina blocks in Early Paleozoic based on the provenance analyses. Sediment inputs eroded from both the Lincang granite and the coeval igneous rocks in the Baoshan and Gongshan blocks were the dominant contributions to the Jurassic strata after the amalgation of the Baoshan and Simao–Indochina blocks. Tectonic processes linking dispersion of the Baoshan–Sibumasu terrane from the Gondwana supercontinent to the collision with the Simao–Indochina block and the deposition of the Cambrian to Jurassic sedimentary sequences were reconstructed." @default.
• W2016690206 created "2016-06-24" @default.
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• W2016690206 date "2015-06-01" @default.
• W2016690206 modified "2023-10-07" @default.
• W2016690206 title "Detrital zircon record of Paleozoic and Mesozoic meta-sedimentary strata in the eastern part of the Baoshan block: Implications of their provenance and the tectonic evolution of the southeastern margin of the Tibetan plateau" @default.
• W2016690206 cites W1522287446 @default.
• W2016690206 cites W1856573459 @default.
• W2016690206 cites W1964092230 @default.
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• W2016690206 cites W1970363584 @default.
• W2016690206 cites W1971606484 @default.
• W2016690206 cites W1971871493 @default.
• W2016690206 cites W1979863090 @default.
• W2016690206 cites W1980480753 @default.
• W2016690206 cites W1982109421 @default.
• W2016690206 cites W1985647492 @default.
• W2016690206 cites W1987420829 @default.
• W2016690206 cites W1992561352 @default.
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• W2016690206 cites W2001391944 @default.
• W2016690206 cites W2004780129 @default.
• W2016690206 cites W2011933206 @default.
• W2016690206 cites W2014398909 @default.
• W2016690206 cites W2014970519 @default.
• W2016690206 cites W2019748000 @default.
• W2016690206 cites W2020973699 @default.
• W2016690206 cites W2022306719 @default.
• W2016690206 cites W2023917364 @default.
• W2016690206 cites W2029403887 @default.
• W2016690206 cites W2030056256 @default.
• W2016690206 cites W2034130965 @default.
• W2016690206 cites W2034397592 @default.
• W2016690206 cites W2039627405 @default.
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• W2016690206 cites W2060461428 @default.
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• W2016690206 cites W2073474967 @default.
• W2016690206 cites W2077411240 @default.
• W2016690206 cites W2078590797 @default.
• W2016690206 cites W2080012412 @default.
• W2016690206 cites W2080611925 @default.
• W2016690206 cites W2080719977 @default.
• W2016690206 cites W2084045184 @default.
• W2016690206 cites W2088845927 @default.
• W2016690206 cites W2089693227 @default.
• W2016690206 cites W2092063385 @default.
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• W2016690206 doi "https://doi.org/10.1016/j.lithos.2015.04.009" @default.
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