K-shape structure is a kind of geological structure recently proposed which is of importance to exploring for mine, but it is necessary to study theoretically the mechanical mechanism of its origin.

Mechanism of K type construction formation and seeking for coal;

Late Cenozoic structural deformation and its implication for petroleum accumulation in the southern Junggar thrust belt;

Features of the pre-Sinian structural deformation in North Jiangxi and its dynamic significance;

Effect of special plastic deposition body on structural deformation and trap forming in western of Kuche Depression.;

The influence of the arcuate structure in .

It takes the form of juxtaposed arcuate structure toward NE orientation, with east wing convergenced toward NE orientation and west wing scattered toward NW orientation.

Xiabaozuo arcuate structure has an eastward salient with NWW and SW ward scatter Regional Marqu Maqn fault(Heye fault) forms its northern boundary It consists of a series of folds and faults in which metamorphic sandy slate of the Xikang Group was involved The arcuate structure was formed by Indosinian and Yanshan movement and gold mineralization is confined to major fault

Features of early-stage tectonic deformation of the Xileng Formation-complex in the Zhangbaling area, Anhui Province;

Late Cenozoic tectonic deformation history and uplift process of the Panxi region,western Sichuan;

Studies on Tectonic Deformation of the Yellow River Terrace in Lanzhou Based on High-resolution GPS Surveying;

Because the geomechanical environment in the northeastern area of Sichuan basin is complicated and unstable,the combination of structural features is special,especially the planar structural feature.

Basing on the formation and characteristic of the oil storage structure in Lamadian, this paper discusses the evolution and formation process of various types of geologic structural feature in the geohistorical background of Daqing Placanticline structure and special mechanic support.