financially and technically supported by the University of Birjand under Project Number 7912.
The eastern Iranian range,known as the Sistan suture zone in the past,has recently been identified as the Sistan orogen.This Paleogene orogeny is located between the Lut and Afghan microcontinents.The structural analy...
funded by the National Natural Science Foundation of China (Nos.42172257,41672199,41421002);MOST Special Fund from the State Key Laboratory of Continental Dynamics,Northwest University;the Foundation of Shaanxi Educational Committee (No.16JK1753)。
The Daba Shan orocline is located at the northeastern margin of the Sichuan Basin and has been inferred as a foreland thrust-fold belt of the Qinling Orogen since the Late Triassic.A complete understanding of rock exh...
supported by the National Natural Science Foundation of China(41888101,41830216 and 41972225);the National Key Technologies R&D Program of China(2017YFC0601305,2018YFE0204202 and 2018YFC0603702);the Geological Survey Program of China(DD20190685)。
Tracing the closure of oceans with irregular margins and the formation of an orocline are crucial for understanding plate reconstruction and continental assembly.The eastern Central Asian Orogenic Belt,where the Mongo...
the ISES post-doctoral grant to DPG(Project No.WA.146101.2.656).
The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen,suturing Gondwana and Laurussia during the Carboniferous.From all swirls of this orogen,a double curve in Iberia stands out,the coupled Canta...
This work was supported by Research Council of University of Sistan and Baluchestan,Zahedan,Iran.
At the southeastern part of the SanandajSirjan Zone of Iran, a group of structural elements outline a large-scale arc curvature around a vertical axis. This curvature comprises several elongated structural elements an...
supported by National Natural Foundation of China(No.41172184);SINOPROBE-08-01;SNOPEC(China)
The Dabashan orocline is situated in the northwestern margin of the central Yangtze block,central China.Previous studies have defined the orthogonal superposed folds growing in its central-western segment thereby conf...
The study was supported by National Natural Foundation of China (No. 41172184);SINOPROBE-08-01;the Institute of Geomechanics Foundation (No.DZLXJK200715)
Many equiaxial dome-like structures developed in the north segment of the Xuefengshan orocline, Central China are obviously inconcordant with the NE-trending linear structures in this area, which contain important rec...
supported by the National Natural ScienceFoundation of China (No. 41172184);SINOPROBE-08-01;SINOPEC
Geofluid, driven by tectonic stress, can migrate and aggregate in geological body. Thus, numerical simulation has been widely used to rebuild paleo-tectonic stress field and probe oil/gas (one type of geofluid) migr...