This study uses clay mineral assemblages, illite "crystallinity'' (IC), chlorite "crystallinity'' (CC), illite polytypes, the b cell-dimension of K-white mica, mineral geothermo-geobarometers and homogenization temperatures of fluid inclusions to investigate the transition from diagenesis to metamorphism in a 7 km thick Triassic flysch sequence in the well Hongcan 1, eastern Tibetan plateau. The 7,012.8 m deep borehole penetrated flysch of Upper to the Middle Triassic age and represents a unique chance to characterize low temperature metamorphic processes in an unusually thick sedimentary sequence developed on thickened continental crust. Mineral assemblage analysis reveals a burial metamorphic pattern with kao...
The Chang 6 reservoir of Yanchang formation in Jingan oilfield has relatively poor quality: the poro...
The Danba Structural Culmination is a tectonic window into the late Triassic to early Jurassic Songp...
Petrologic features, diagenetic processes and origins of different pore types of Upper Triassic Chan...
We used illite and chlorite crystallinities, index minerals, mineral assemblages, polytype and domai...
Low temperature metamorphic indicators were used to investigate the tectonothermal evolution of the ...
The sandstone reservoir experienced diagenesis of compaction, cementation, dissolution, and replacem...
Abstract: In the Manang area a distinctive metamorphic zonation with grade increasing downward to de...
Low-and very low-grade metamorphic studies investigating the alteration and reaction progress of cla...
The eighth member of Upper Triassic Yanchang Formation (Chang 8) is the major oil reservoir unit in ...
Medium to high-grade metamorphic rocks comprising numerous graphite deposits are widely distributed ...
The Dongmozhazhua deposit, the largest Pb–Zn deposit in south Qinghai, China, is stratabound, carbon...
Qaidam Basin is a tectonically controlled Mesozoic-Cenozoic depression on the northern margin of the...
The Mesozoic Chang 8 Section in the Zhenjing area is a typical low permeability-tight sand reservoir...
10 pagesInternational audienceDetailed clay mineralogical analyses were carried out on Late Permian/...
Through a range of petrological techniques, the petrology, diagenesis, pore characteristics, and con...
The Chang 6 reservoir of Yanchang formation in Jingan oilfield has relatively poor quality: the poro...
The Danba Structural Culmination is a tectonic window into the late Triassic to early Jurassic Songp...
Petrologic features, diagenetic processes and origins of different pore types of Upper Triassic Chan...
We used illite and chlorite crystallinities, index minerals, mineral assemblages, polytype and domai...
Low temperature metamorphic indicators were used to investigate the tectonothermal evolution of the ...
The sandstone reservoir experienced diagenesis of compaction, cementation, dissolution, and replacem...
Abstract: In the Manang area a distinctive metamorphic zonation with grade increasing downward to de...
Low-and very low-grade metamorphic studies investigating the alteration and reaction progress of cla...
The eighth member of Upper Triassic Yanchang Formation (Chang 8) is the major oil reservoir unit in ...
Medium to high-grade metamorphic rocks comprising numerous graphite deposits are widely distributed ...
The Dongmozhazhua deposit, the largest Pb–Zn deposit in south Qinghai, China, is stratabound, carbon...
Qaidam Basin is a tectonically controlled Mesozoic-Cenozoic depression on the northern margin of the...
The Mesozoic Chang 8 Section in the Zhenjing area is a typical low permeability-tight sand reservoir...
10 pagesInternational audienceDetailed clay mineralogical analyses were carried out on Late Permian/...
Through a range of petrological techniques, the petrology, diagenesis, pore characteristics, and con...
The Chang 6 reservoir of Yanchang formation in Jingan oilfield has relatively poor quality: the poro...
The Danba Structural Culmination is a tectonic window into the late Triassic to early Jurassic Songp...
Petrologic features, diagenetic processes and origins of different pore types of Upper Triassic Chan...