Origin of natural gas and main controlling factors of reservoirs in Wolonghe Gas Field
The northern Longmenshan front belt extends along Guangyuan to Anxian and includes the typical anticlines such as Kuangshanliang, Tianjingshan, Qinglinkou and Zhongba. Field investigations and seismic interpretation ascertained two episode tectonic deformations in the Late Triassic and the Cenozoic periods in this front belt. The Kuangshanliang and Tianjingshan structures show a duplex comprising of a shallow fault-bend fold in the Late Triassic period and a deep buried stacking anticline imbricated by several thrust sheets in the Cenozoic period. The Qinglinkou and Zhongba structures show a imbricate structure in the Late Triassic and a buried faultbend fold and fault-propagation fold, which may be created or altered in the Cenozoic period. The front belt of the northern Longmenshan exhibits a double-layer structural style characterized by shallow thrust structures and deep buried ones. The buried thrust structures are the frontier fields for hydrocarbon exploration in the northern Longmenshan area.
Characteristics of fault structure and its control to hydrocarbon in Bozhong Depression
According to the reservoir-formation mechanism, exploration situation and potential hydrocarbon resources, the geologic distribution of reservoirs in the fault basins of Jizhong Paleocene and Erlian Early Cretaceous periods were analyzed. In the course of complex geologic evolution, three elements of the fault basin including “sedimentary evolution-sedimentary facies-reservoir facies”, “structural zone-temperature-pressure field-hydrocarbon potential” and “transporting system” were gradually adjusted from the dynamic variation to the static equilibrium. Under the particular geologic condition and 3- dimensional space, six types of relative independent “complex transporting system” were constituted, including fault,ladder-shape, grid, plane, sitting chair and fissure types. Various complex reservoirs or complex reservoir zones were generated in fault basin. This reservoir model is the facies-potential-transport ternary reservoir model. The ternary reservoir model controlled rigorously the regular distribution, enrichment degree and exploration prospect of hydrocarbon in the rich oil trough.
Characteristics and origins of fractures developed in Ordovician reef-bank complex in Shunxi area of central Tarim Basin
Compact-expulsion characteristics of source rocksin Shahejie Formation of Dongying Depression using percolation method
Determination of favorable oil-bearing areas with extra low-permeability reservoir by “dessert” of petro-physical facies
Dynamic pressure analysis on wells with vertical fractures in low-permeability dual-porosity reservoir