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1. Age of Sichuan foreland basin is given.

2. The west sichuan depression a typical Superimposed foreland basin.

3. Is Jurassic Chaidamu Basin a Foreland Basin?

4. In the foreland basin sediment environment, the transilient group of mud rock and sandstone are the main sediment features of low-stand system tract.

5. Searching salt diapers and related traps in Kuqa foreland basin is important.

6. In fact, the prosperity of Chinese foreland had expanded stagestage inland area.

7. The overthrust fault zone and foreland basin in Southwestern Tarim is favorable areas for petroleum exploration. But the research and exploration degree here are still low.

8. The foreland of Daba Mountains resulted from the intracontinental orogeny of the Qingling orogenetic movements.

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9. Therefore , foreland basin becomes the favorable place for reservoir.

10. From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

11. Foreland basins are important areas of exploration for petroleum in China.

12. In foreland, the exchange scale and quantities of the collective construction land by remise, demise, rent and mortgage are very tremendous.

13. Foreland is concentration of Fujian Province population, economy developeds area.

14. Because the foreland basin was a highly subsidence, that it was deposited a hugely Plio - Pleistocene sediments.

15. The interstice of foreland slope was mainly dissolved pore and some primary pore.

16. Foreland thrust belts are developed extensively margin of Meso Cenozoic sedimentary basins in northwestern China.

17. Foreland basin is one type of the most prolific petroliferous basins in the world, where thrust belt is one of its most abundant plays.

18. The basin between orogenic belt and craton is called foreland basin.

19. To some extent, the facies evolution reflects the tectonic controls on the sedimentation of foreland basin.

20. There are different depositional fillings and stratigraphic patterns on the ambilateral sides of the foreland basin during the stage of tectonic activity and stability.

21. The tectonic subsidence is the main controlling factor in the foreland basin, which went through three periods, namely press, flexure subsidence to laxitas, uplift.

22. From the Cretaceous, Tarim basin began the new evolutional stage of foreland basin.

23. It controlled the formation, deformation of the Meso- Cenozoic Tarim and Qaidam foreland basins, in which the hydrocarbon accumulation was influenced.

24. It is suggested that thrusts with nearly E-W strike direction and southward-dipping direction were developed in the pre-Jurassic basement of the basin during foreland deformation in Indosinian.

25. Closing of Tethys and continuous compressing and squeezing of Indian plate were the tectonic dynamics background for the formation of foreland basins in western China.

26. NE Sichuan basin went through the transformational history from large fresh water depression basin after inland craton to foreland basin of Daba mountain.

27. Himalayan movement made the area developed as a para - foreland basin.

28. The lithologic oil and gas reservoirs are developed in the foreland thrust fault zones due to highly structural activity.

29. The gases are mainly distributed in cratonic uplift, fault belts and fault - folded belts of foreland basin.

30. Tarim basin is a huge superposed basin composed of Paleozoic cratonic basin and Meso - Cenozoic foreland basin.