The Southern Atlas front of Tunisia(SAFT),which includes the Gantass structure,is part of the wide fold and thrust belt that developed along the North African margin.In the present work,an integrated geological and ge...
Supported by the National Natural Science Foundation Project of China(U22B6002);Prospective Basic Technology Research Project of PetroChina(2021DJ0605).
Based on outcrop,seismic and drilling data,the main regional unconformities in the Sichuan Basin and their controls on hydrocarbon accumulation were systematically studied.Three findings are obtained.First,six regiona...
The Tunisian Dorsal backland is the Eastern Atlas side of maghrebides. Field data of Fahs area allowed us to develop new interpretations and to characterize the main structural features of the studied devices (Jebel R...
financially supported by the National Science and Technology Major Project(Grant No.2011ZX05008-001);the National Natural Science Foundation of China(Grant No.40739906);the Chinese State 973 Project(Grant No.2011CB201100)
The Hala'alat Mountains are located at the transition between the West Junggar and the Junggar Basin. In this area, rocks are Carboniferous, with younger strata above them that have been identified through well data ...
Research Area comprises of Punjab Monocline, Sulaiman Foredeep and Eastern Part of Sulaiman Fold Belt (from east to west) in Central Indus Basin, Pakistan. Sargodha High is located in northeast of a Seismic Profile AB...
Several stratigraphic breaks and unconformities exist in the Mesoproterozoic successions in the northern margin of the North China Block. Geologic characters and spatial distributions of five of these un- conformities...
supported by the National Natural Science Foundation of China(No.41130422);the National Basic Research Program of China(Nos.2011CB201100-03 and 2006CB202302);the Frontier Research Project of Marine Facies of the Oil Industry in China
The Tarim basin experienced a complex tectonic evolutionary history from Sinian to Ceno zoic. Eight largescale and more than 20 subordinate unconformities defining tectonosequences of dif ferent protobasins formed in ...
Well logs and biostratigraphic data from six wells in the “XB Field”, central Swamp Depobelt, Niger Delta were integrated to carry out a sequence stratigraphic analysis of depositional systems in the field. The anal...
Strata erosion is a widespread phenomenon in sedimentary basins. The generation, migration, and accumulation of hydrocarbon is influenced by the scale of erosion, so estimating the amount of erosion is essential in th...
The formation process of the Dianqiangui basin, a special basin, occurred after the Caledonian orogeny, in the south of Guizhou, the west of Guangxi and the southeast of Yunnan, experienced three periods: it began ...