The geological conditions and exploration potential of shale oil in Chang7 Member, Upper Triassic Yanchang Formation, Ordos Basin, were studied from various aspects, including petrographic characteristics, storage ability, geochemical features, friability and mobility of hydrocarbon in the source rock, etc. A classification criterion of lithofacies for Upper Triassic Chang 7 source rock in Ordos Basin were established based on the correlation between lithology, organic carbon content and logging parameters, from which, the spatial distribution and development scale of two types of shale, black shale and dark massive mudstone, have been predicted. Qualitative and quantitative characterization of the micro-structures of Chang7 source rock usi...
AbstractThis paper presents a case study of lacustrine organic-rich shale from the Yanchang Formatio...
The assessment of shale gas potential for the Ordovician Pingliang Formation and Carboniferous–Permi...
The Yanchang Formation was deposited in a terrestrial environment in the late Triassic period. It co...
Abstract The Ordos Basin is the largest petroliferous basin in China, where the Chang 7 Member shale...
Following the successful exploration of shale oil in North America, China recently started to explor...
In the Triassic Yanchang Formation, Jiyuan-Wuqi area, Ordos Basin, the Chang 6 reservoir is contacte...
<p>The Chang 7 Member of the Yan-Chang Formation (Yan-Chang #7 Member), which is located in the cent...
Shale oil is an unconventional oil resource that needs to be developed and utilized urgently. Howeve...
The geological characteristics of Mesozoic lacustrine shale gas are summarized from the following as...
By comprehensive study of reservoir and source rock distribution, petrology and geochemistry, the ti...
The Chang7 Member of the Triassic Yanchang Formation in the Ordos Basin is a typical continental tig...
The Chang 6 reservoir of Yanchang formation in Jingan oilfield has relatively poor quality: the poro...
The study of the oil shale from Triassic Chang 7 oil layer in Ordos Basin is of great importance to ...
The study of the oil shale from Triassic Chang 7 oil layer in Ordos Basin is of great importance to ...
New discoveries have been achieved in the exploration of the Yanchang Formation Chang 9 member. This...
AbstractThis paper presents a case study of lacustrine organic-rich shale from the Yanchang Formatio...
The assessment of shale gas potential for the Ordovician Pingliang Formation and Carboniferous–Permi...
The Yanchang Formation was deposited in a terrestrial environment in the late Triassic period. It co...
Abstract The Ordos Basin is the largest petroliferous basin in China, where the Chang 7 Member shale...
Following the successful exploration of shale oil in North America, China recently started to explor...
In the Triassic Yanchang Formation, Jiyuan-Wuqi area, Ordos Basin, the Chang 6 reservoir is contacte...
<p>The Chang 7 Member of the Yan-Chang Formation (Yan-Chang #7 Member), which is located in the cent...
Shale oil is an unconventional oil resource that needs to be developed and utilized urgently. Howeve...
The geological characteristics of Mesozoic lacustrine shale gas are summarized from the following as...
By comprehensive study of reservoir and source rock distribution, petrology and geochemistry, the ti...
The Chang7 Member of the Triassic Yanchang Formation in the Ordos Basin is a typical continental tig...
The Chang 6 reservoir of Yanchang formation in Jingan oilfield has relatively poor quality: the poro...
The study of the oil shale from Triassic Chang 7 oil layer in Ordos Basin is of great importance to ...
The study of the oil shale from Triassic Chang 7 oil layer in Ordos Basin is of great importance to ...
New discoveries have been achieved in the exploration of the Yanchang Formation Chang 9 member. This...
AbstractThis paper presents a case study of lacustrine organic-rich shale from the Yanchang Formatio...
The assessment of shale gas potential for the Ordovician Pingliang Formation and Carboniferous–Permi...
The Yanchang Formation was deposited in a terrestrial environment in the late Triassic period. It co...