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Technical analysis by comparing the Taipei basin, Turpan Depression, pore characteristics and effectiveness

Close relationship with the layer plane. Effective with the main focus of secondary porosity in the Jurassic, the tectonic changes with the corresponding greater depth. To be further explored with the second secondary porosity. Is \ Wins the North, the East sub-concave hill secondary larvae L gap for secondary development zone, which determines the degree of development of larvae deep reservoir the effectiveness of L gap. Reservoir distribution in the fracture system of quality development, hydrocarbon migration point, near the source rocks developed areas along the Flaming Mountain fault zone is to find high-quality reservoir exploration. References: 1] Yuan Ming,[link widoczny dla zalogowanych],, Liang Shijun, Yan Can the column, and so on. Leaf-Hami basin petroleum geology and exploration practice [M]. Beijing: Petroleum _r, 【kH {University Press, 20O2 :3-321.: 2] Wu Tao. Zhao. Ⅲ-Hami Basin coal gas leaves the formation and distribution of [M]. Beijing: Petroleum Industry Press _I II. 1997; BU 268. f3] Yuan Ming. Turpan-Hami Basin oil and gas distribution and exploration direction [J]. Xinjiang Petroleum Geology, 1998,19 (2): 106III. 4] Zhao Changyi. Zhao, Cheng KM, et al. Turpan-Hami Basin and kerosene oil -generating source rock evaluation of the conditions J]. Petroleum Technology, 1998.19 (3) :21-25. j] Cheng KM. Ying Xiong, who Xiaoming, et al. Turpan-Hami Basin coal into hydrocarbons [J]. Petroleum Technology , 2002.23 (4) :13-17. [6] Shou peak. Chu Wai Wah. Quantitative preservation of porosity in sandstone prediction [J]. Geological Sciences. I99 {4,[link widoczny dla zalogowanych],32 (2): 244246.7] status of the military, Tang Yong. Zhu Guohua, et al. Junggar Basin, the Jurassic reservoirs of the basic features of the master? Cable [J]. Petroleum Exploration and Development, 2000,29 (I) :52-55. Es] AlaaM, SalemS, MoradS, eta1.1) iagenesisandreservoir ・ qualityevo [uti ~ noffluvialsandstonesduringprogressiveburiMandup-lift: EvidencefromtheUpperJurassicBoipehaMember, Recon-cavoBasin. NortheasternBrazil [J]. AAPGBulletin, 2000,84 (7): 10I51040. uPaxtonST, SzaboJ (). Calvert 【, S, eta1 . PreservationofprimaryporosityindeepIyburiedsandstones: Anewplayconceptfromthe (TretaceousTuscaloosaSandstoneofLouisiana [J]. AAPGBuIledn, 1990,74 (6) :737-74I .1 (}] Luo Jinglan. ZHANG Xiao. Zhangyun Xiang, et al. Diagenesis as, ElJ river deltaic sandstones of the evolution of reservoir properties [J]. Deposition of .200 I.I9 (4): 54I a 546.11] Li M C.. Oil e basic theory of migration oil and gas exploration EJ3. Earth Sciences,[link widoczny dla zalogowanych], a China University of Geosciences. 2004.24 (4 ): 379 - 383. [12JPratschJDeterminationofexplorationbymigrationpathwaysofoilandgasU]. ForeignOilandGasExploration. 1997.9 (1) :63-68. f13] Hou Ping, cycles. Luo XR. left foot i = time migration paths of oil pattern analysis [J]. [{】 National Science I) series. 2004.34 (Supplement T) :162-168. [14] by less. OF SCIENTIFIC Shou Feng, other towers in the northern slope of the Silurian uplift reservoir characteristics and control Gangsuo [J]. Chengdu management 『= University : fj natural Science,[link widoczny dla zalogowanych], 2004,31 (2): 148152. [15] Fu Guang, Pang,[link widoczny dla zalogowanych], Yang Mian, et al. H states of natural gas migration and its significance card [J]. China Offshore Oil (Geology), 2000 , 14 (2) :112-116. (2) Taipei Jurassic reservoir depth was generally effective lower limit (Received 20,050,328 back to the date of 2OO5.0904 Editor Zhang Yi)
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