It is pointed out that the aggregation and collision of the numerous diverse micro-cratons is the dynamic genesis of the foreland basin group in the central and western China, which also caused the diversity and particularity of these forelan.

Hence,the distribution of oil and gas is controlled by the paleo-uplift in the small cratonic basins and thrust fold belts in the foreland basins in the Tarim basin,which resulted in the formation of oil and gas accumulation of voluminous litho-strata and anticlase,respectivelg.

Re-Os isotopic analysis of the Kalatongke Cu-Ni Sulfide Deposit,Northern Xinjiang,NW China,and its geological implication.;

Geochemistry of the Kalatongke basic complex in Xinjiang and its constraints on genesis of the deposit;

Petrogenesis of Kalatongke Cu-Ni sulfide deposit in Xinjiang

Prospects of exploring Palaeozoic primary oil and gas pools in southern area of North China cratonic basin;

Formation mechanism and tectonic types of intracratonic paleo-uplifts in the Tarim basin;

Relationship between gas carbon isotope and maturity in cratonic basin, Tarim Basin;

Correctly discriminating and differentiating the cratonization will help us to deeply understand the formation and evolution of the continental lithosphere.

Regional geological structural evolution in Shandong province can be divided into 5 stages:① nuclear area forming stage: Archaean high-grade area formed, crust differentiated into stable granite arch and active greenstone belts, and the first cratonization completed.

The results reveal that the Guandi complex underwent high-grade regional metamorphism and anatexis in the late Neoarchaean,which provides further metamorphic chronological evidence for cratonization of the the Eastern North China block.