Dolostones of tidal flat facies are the major reservoir rock type of the fourth member of Leikoupo
Formation, Longmen Mountain front, western Sichuan Basin. The reservoir controls are …

… between the Sichuan Basin, … the Longmen Shan Foreland Basin, which contains an Upper
Triassic megasequence related to Indosinian deformational events in the adjacent Longmen …

… Longmen Shan rises to more than 6 km (3.7 mi) above the Sichuan Basin, forming one of the
steepest mountain fronts … that the steep topographic front of the Longmen Shan results from …

… likely to find large-scale reef flat karst gas pools in the trap structural belt in the Longmen
Mountain front in SW Sichuan Basin and in the slope belt in the western Sichuan Depression. …

… the Sichuan basin within the foothills of the southern Longmen Shan. The QTF has a distinctive
north–south (N–S) trend that is oblique to the northeast (NE)‐trending southern Longmen …

… Plateau adjacent to the Sichuan basin, is characterized by … portions of the Longmen Shan
and western Sichuan basin to … and southern Longmen Shan and the western Sichuan basin …

… The southern Longmen Shan region has … front due to thrusting from a shallow décollement.
The concurrent faulting at the rear and at the front is separated by the flat Sichuan Basin. The …

… (b) Three-dimensional model of the Range Frontal blind thrust and Longquan fault system
in the Longmen Shan and Sichuan basin. This model is modified from the previous results of …

… , the Longmen Shan has probably been a region of elevated topography relative to the Sichuan
Basin … to the Sichuan Basin since this time. The fact that Upper Triassic marginal foreland …

… Longmen Shan. It marks the southeastern most edge of the eastern margin of the Tibetan
Plateau (EMTP) and towers above the Sichuan Basin … focused on the Longmen Shan orogen, …