Results 151 to 160 of about 1,509,261 (248)
Abstract The timing of Cenozoic deformation in the East Kunlun Mountains, northern Tibet, is crucial for understanding plateau growth but remains disputed due to the scarcity of direct chronological constraints on specific tectonic structures. Here, we present a high‐density‐sampling magnetostratigraphic record from the Xiaohongshan section, interior ...
Leyi Li +3 more
wiley +1 more source
Distribution of Vanadium in the Upper Permian Coal of the Northwest Guizhou Area: What Affects This Distribution? [PDF]
Chen L, Wu Z, Tian F, Zhao L, Wei Y.
europepmc +1 more source
Study on the Micro-Nano Characteristics of Organic-Rich Shale Reservoirs Under Differential Sedimentation: A Case Study of the Lower Silurian Longmaxi Formation and Upper Permian Dalong Formation Shales in the Sichuan Basin, China. [PDF]
Wang J +7 more
europepmc +1 more source
The tetrapod fauna of the upper Permian Naobaogou Formation of China: 3. Jiufengia jiai gen. et sp. nov., a large akidnognathid therocephalian. [PDF]
Liu J, Abdala F.
europepmc +1 more source
A new moradisaurine captorhinid reptile (Amniota: Eureptilia) from the upper Permian of India. [PDF]
Reisz RR, Chatterjee S, Modesto SP.
europepmc +1 more source
The Upper Permian Mizukoshi Formation
openaire +2 more sources
Permianella (Brachiopoda) from the Upper Permian of Transcaucasia
A species of Permianella He and Zhu, Permianella grunti n. sp., is described for the first time from the Araxoceras Bed of the Dzhulfa Formation in the Dorasham II section, Transcaucasia. This record shows the westernmost distribution of permianellids.
openaire +1 more source
The Permian System in the Netherlands is subdivided into the Lower Rotliegend, Upper Rotliegend and Zechstein groups. These groups were deposited in a large epicontinental basin extending from the UK to Poland.
Geluk, M.C., Bouroullec, R., Geel, C.R.
core
The Middle-Upper Permian marine shale formations in the middle Yangtze region are an important replacement field for shale gas exploration and development in China, with great resource potential. However, their reservoir development is complex.
KONG WEILIANG +10 more
doaj
Data obtained on conodont distribution in the Permian-Triassic Sovetashen Section of Transcaucasia provide further limitations on the age of the carbon-isotopic anomalies discovered by Baud et al. (1989).
Kozur, H +3 more
core

