The states of S species in black shares are very complex,such as organic sulfur, pyrite sulfur and sulphate sulfur, The mineral microtexture, sulfur content and sulfur isotope can indicate the formation conditions and diagenetic processes of the black shales. The S species are separated perfectly and the relation between the content, mineral microtexture and sulfur isotope composition of the sulfur mineral is assessed. These complementary approaches provide people a new insight into the formation conditions of the black shales and redox conditions of Precambrian and Cambrian in Southwest China.Multidisciplinary SciencesSCI(E)1ARTICLE171612-16164
Two hundred and fifty-nine sulphide samples from black shales of the 'Productive' Formation belongin...
The first studies on sulfur isotope geochemistry were performed approximately sixty years ago (e.g.,...
Over 200 samples of mid-Cretaceous organic-rich sediment were examined to determine abundance and is...
The organic sulfur compounds were isolated from an immature shale oil in Hetao Basin, northern China...
Integrated analysis of whole-rock and mineral geochemical data from black shale and metamorphosed bl...
Sulphides can be divided into two major groups, those which are of hydrothermal origin and those whi...
The lacustrine black shales in the Chang7 Member from the Upper Triassic Yanchang Formation of the O...
Pyrite bearing barite concretions are abundant in black shales of the Early Cambrian Niutitang Forma...
Pyrite bearing barite concretions are abundant in black shales of the Early Cambrian Niutitang Forma...
Pyrite bearing barite concretions are abundant in black shales of the Early Cambrian Niutitang Forma...
The content and isotopic composition of pyrite sulfur are significantly affected by local deposition...
Mass-independent fractionation of sulfur isotopes found in Early Precambrian records is the main evi...
Sulfur isotopic ratios were measured on about a dozen suites of co-existing sulfide minerals from so...
The copper ores at Mount Isa (Queensland, Australia) are hosted by the Urquhart Shale, a metamorphos...
The sulfur isotopic record of sedimentary sulfides (mainly pyrite) and sulfates shows considerable v...
Two hundred and fifty-nine sulphide samples from black shales of the 'Productive' Formation belongin...
The first studies on sulfur isotope geochemistry were performed approximately sixty years ago (e.g.,...
Over 200 samples of mid-Cretaceous organic-rich sediment were examined to determine abundance and is...
The organic sulfur compounds were isolated from an immature shale oil in Hetao Basin, northern China...
Integrated analysis of whole-rock and mineral geochemical data from black shale and metamorphosed bl...
Sulphides can be divided into two major groups, those which are of hydrothermal origin and those whi...
The lacustrine black shales in the Chang7 Member from the Upper Triassic Yanchang Formation of the O...
Pyrite bearing barite concretions are abundant in black shales of the Early Cambrian Niutitang Forma...
Pyrite bearing barite concretions are abundant in black shales of the Early Cambrian Niutitang Forma...
Pyrite bearing barite concretions are abundant in black shales of the Early Cambrian Niutitang Forma...
The content and isotopic composition of pyrite sulfur are significantly affected by local deposition...
Mass-independent fractionation of sulfur isotopes found in Early Precambrian records is the main evi...
Sulfur isotopic ratios were measured on about a dozen suites of co-existing sulfide minerals from so...
The copper ores at Mount Isa (Queensland, Australia) are hosted by the Urquhart Shale, a metamorphos...
The sulfur isotopic record of sedimentary sulfides (mainly pyrite) and sulfates shows considerable v...
Two hundred and fifty-nine sulphide samples from black shales of the 'Productive' Formation belongin...
The first studies on sulfur isotope geochemistry were performed approximately sixty years ago (e.g.,...
Over 200 samples of mid-Cretaceous organic-rich sediment were examined to determine abundance and is...