This research was supported by the Korea Institute of Energy Technology Evaluation and Planning(KETEP)grant(no.20212010200020);the Energy&Mineral Resources Develop-ment Association of Korea(EMRD)grant(Datascience based oil/gas exploration consortium),funded by the Ministry of Trade,Industry&Energy(MOTIE)of the Republic of Korea.
Transpression occurs in response to oblique convergence across a deformation zone in intraplate regions and plate boundaries.The Korean Peninsula is located at an intraplate region of the eastern Eurasian Plate and ha...
Recent petro-structural investigations on the Faboula gold deposit located in the Bougouni-Kékoro basin, in southern Mali, north-west of the Leo-Man Shield, have provided new data on the nature and spatial organizati...
Transpressional deformation has played an important role in the late Neoproterozoic evolution of the ArabianNubian Shield including the Central Eastern Desert of Egypt.The Ghadir Shear Belt is a 35 km-long,NW-oriented...
supported by University of Sistan and Baluchestan and the Shiraz University Research Council (SURC)
Radiolarites have an important role in the reconstruction of the paleogeography, bathymetry and their coexistence with ophiolites gives an opportunity to determine the tectonic his- tory of collisional zones. The radi...
Dena Fault is one of the fundamental and main structures with more than 130 km. One of the most important structural properties of this fault is changing in its trend so that at least three structural trends are detec...
supported jointly by the China Geological Survey project(grant number:1212011120167,12120114002201);China National Natural Science Foundation(grant number 41472178)
We present in this paper some new evidence for the change during the Quaternary in kinematics of faults cutting the eastern margin of the Tibetan Plateau. It shows that significant shortening deformation occurred duri...
Oblique continent—continent collision between Iranian microcontinent and Arabian plate is the main cause of transpression and transtension regimes in this area. Zagros orogeny in this area resulted in formation of va...
The western part of the Kedougou Kenieba Inlier is located in the West African Craton. It consists of paleoproterozoic NE-trending elongate belts (subprovinces) of metavolcanic and granitic rocks that alternate with m...
Supported by National Natural Science Foundation of China (Grant Nos. 40802050, 49802020, 40172074);China Postdoctoral Science Foundation (Grant No. 20070440065)
This work deals with the preliminary relationship between strain path and strain partitioning pattern in a sinistral transpressional zone, Lancangjiang shear zone, located to the southeast of Tibet. Various ductile ro...
This work was supported by the State Key Basic Research Development Project (Grant No. G1998040800).
A special extended basin topography is developed in the middle segment of the Altyn Tagh Fault Zone. The ratio of its length to width is over 50. The long boundaries at the two sides of the basin are controlled by the...