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- W3007118869 endingPage "103431" @default.
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- W3007118869 abstract "The geochemistry of source rock–controlled coals from the Late Triassic Daqiaodi Formation in the Dabaoding Coal Mine of the southwestern Sichuan Province was investigated. A total of 15 coal samples, 6 parting samples, and 4 roof and floor rock samples from the D15–3 and D18 coals were subjected to proximate and ultimate analyses for coal quality, by using LTA-XRD with Siroquant software for minerals, XRF for major element oxides, ICP-MS for trace elements, ICP-CCT-MS for As and Se, ISE for F, and a DMA-80 analyzer for Hg. Results indicate that the Dabaoding D15–3 and D18 coals are classified as low ash and low-volatile bituminous coal. Minerals in coals are dominated by quartz, kaolinite, illite, and dolomite. Most trace elements in the Dabaoding coals are depleted or at normal levels relative to Chinese coals or world hard coals (except for Cr with slight enrichment). The Dabaoding coals and host rocks are characterized by weakly positive Ce and Y anomalies, strongly positive Gd anomalies, and weakly negative Eu anomalies. Based on paleogeographical, mineralogical, and geochemical evidence, the sediment source rocks of the Daqiaodi coal-bearing strata are identified as the Panzhihua trachyte at the top of the Kangdian Upland, which exerted crucial impacts on the Dabaoding coals." @default.
- W3007118869 created "2020-03-06" @default.
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- W3007118869 date "2020-03-01" @default.
- W3007118869 modified "2023-10-17" @default.
- W3007118869 title "Geochemistry of source rock–controlled Late Triassic coal: An example from the Dabaoding Coal Mine in Panzhihua, Sichuan Province, southwestern China" @default.
- W3007118869 cites W1162175410 @default.
- W3007118869 cites W1963574048 @default.
- W3007118869 cites W1965778247 @default.
- W3007118869 cites W1966174256 @default.
- W3007118869 cites W1974356108 @default.
- W3007118869 cites W1975407111 @default.
- W3007118869 cites W1977552998 @default.
- W3007118869 cites W1981316911 @default.
- W3007118869 cites W1982616497 @default.
- W3007118869 cites W1983297630 @default.
- W3007118869 cites W1983734980 @default.
- W3007118869 cites W1984264571 @default.
- W3007118869 cites W1985993860 @default.
- W3007118869 cites W1987882813 @default.
- W3007118869 cites W1987974104 @default.
- W3007118869 cites W1988114452 @default.
- W3007118869 cites W1992245388 @default.
- W3007118869 cites W1992292460 @default.
- W3007118869 cites W1993489621 @default.
- W3007118869 cites W1996569492 @default.
- W3007118869 cites W1999448338 @default.
- W3007118869 cites W2005100095 @default.
- W3007118869 cites W2007975985 @default.
- W3007118869 cites W2011528281 @default.
- W3007118869 cites W2013259970 @default.
- W3007118869 cites W2013867612 @default.
- W3007118869 cites W2016532831 @default.
- W3007118869 cites W2017723471 @default.
- W3007118869 cites W2019040497 @default.
- W3007118869 cites W2019737722 @default.
- W3007118869 cites W2023759362 @default.
- W3007118869 cites W2027069634 @default.
- W3007118869 cites W2030281083 @default.
- W3007118869 cites W2031194632 @default.
- W3007118869 cites W2035680956 @default.
- W3007118869 cites W2037865108 @default.
- W3007118869 cites W2038183458 @default.
- W3007118869 cites W2038201589 @default.
- W3007118869 cites W2039380792 @default.
- W3007118869 cites W2041080800 @default.
- W3007118869 cites W2041157551 @default.
- W3007118869 cites W2041383962 @default.
- W3007118869 cites W2043621358 @default.
- W3007118869 cites W2045405837 @default.
- W3007118869 cites W2049900380 @default.
- W3007118869 cites W2053618511 @default.
- W3007118869 cites W2054712097 @default.
- W3007118869 cites W2057063592 @default.
- W3007118869 cites W2059451312 @default.
- W3007118869 cites W2064493626 @default.
- W3007118869 cites W2069532814 @default.
- W3007118869 cites W2075910519 @default.
- W3007118869 cites W2076800691 @default.
- W3007118869 cites W2078617700 @default.
- W3007118869 cites W2080227270 @default.
- W3007118869 cites W2080860526 @default.
- W3007118869 cites W2082921028 @default.
- W3007118869 cites W2084239657 @default.
- W3007118869 cites W2086490840 @default.
- W3007118869 cites W2087234724 @default.
- W3007118869 cites W2087533922 @default.
- W3007118869 cites W2088997939 @default.
- W3007118869 cites W2090249742 @default.
- W3007118869 cites W2093750105 @default.
- W3007118869 cites W2094725054 @default.
- W3007118869 cites W2103509464 @default.
- W3007118869 cites W2106533331 @default.
- W3007118869 cites W2111119089 @default.
- W3007118869 cites W2121221338 @default.
- W3007118869 cites W2127201333 @default.
- W3007118869 cites W2149374208 @default.
- W3007118869 cites W2181469240 @default.
- W3007118869 cites W2219663543 @default.
- W3007118869 cites W2322370948 @default.
- W3007118869 cites W2342348073 @default.
- W3007118869 cites W2468230850 @default.
- W3007118869 cites W2469045433 @default.
- W3007118869 cites W2489561826 @default.
- W3007118869 cites W2496781418 @default.
- W3007118869 cites W2510917724 @default.
- W3007118869 cites W2568430364 @default.