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To build the palaeo-redox environment model of the Longmaxi Formation shale during the Silurian Rhuddanian stage in Southern Sichuan Basin, China, 20 core samples taken from wells W201 and N1 were determined by carbon-sulphur analyser, X-ray fluorescence (XRF) spectrometry, and inductively coupled plasma-mass spectrometry (ICP-MS) to test for the major and trace elements. Major elements test results shows that fragile mineral SiO 2 component and degree of total pyritization in section A isdoi:10.2306/scienceasia1513-1874.2018.44.109 fatcat:tff2ud5qefdqhbknbxr65mkmgy