[1] Clough G W, Sitar N, Bachus R C, et al.Cemented sands under static loading[J].Journal of the Geotechnical Engineering Division, 1982, 107(6):799-817.
[2] Karig D E, Hill I A, Taira A, et al.Reconsolidation tests and sonic velocity measurements of clay-rich sediments from the Nankai Trough[J].Proceedings of the Ocean Drilling Program, Scientific Results, 1993, 131:247-260.
[3] Ehrenberg S N.Preservation of anomalously high porosity in deeply buried sandstones by grain-coating chlorite:examples from the Norwegian Continental Shelf[J].AAPG Bulletin, 1993, 77(7):1260-1286.
[4] Zhu S F, Zhu X M, Wang X L, et al.Zeolite diagenesis and its control on petroleum reservoir quality of Permian in northwestern margin of Junggar Basin, China[J].Science China:Earth Sciences, 2012, 55(3):386-396.
[5] 朱国华.陕北浊沸石次生孔隙砂体的形成与油气关系[J].石油学报, 1985, 6(1):1-8.
Zhu Guohua.Formation of lomonitic sand bodies with secondary porosity and their relationship with hydrocarbons[J].Acta Petrolei Sinica, 1985, 6(1):1-8.
[6] Surdam R C, Sheppard R A.Zeolites in saline, alkaline-lake deposits[M]//Sand L B, Mumpton F A.Natural Zeolites:Occurrence, Properties, Use.New York:Pergamon Press, 1987:145-174.
[7] Surdam R C, Crossey L J, Hagen E S, et al.Organic-inorganic interactions and sandstone diagenesis[J].AAPG Bulletin, 1989, 73(1):1-23.
[8] Zhu Shifa, Zhu Xiaomin, Niu Huapeng, et al.Genetic mechanism of dolomitization in Fengcheng Formation in the Wu-Xia area of Junggar Basin, China[J].Acta Geologica Sinica:English Edition, 2012, 86(2):447-461.
[9] Morad S, Bergan M, Knard R, et al.Albitization of detrital plagioclase in Triassic reservoir sandstones from the Snorre Field, Norwegian North Sea[J].Journal of Sedimentary Petrology, 1990, 60(3):411-425.
[10] 王宏语, 樊太亮, 肖莹莹, 等.凝灰质成分对砂岩储集性能的影响[J].石油学报, 2010, 31(3):432-439.
Wang Hongyu, Fan Tailiang, Xiao Yingying, et al.Effect of tuffaceous components on physical property of sandstone reservoir[J].Acta Petrolei Sinica, 2010, 31(3):432-439.
[11] Jiao Yangquan, Yan Jiaxin, Li Sitian, et al.Architectural units and heterogeneity of channel reservoirs in the Karamay Formation, outcrop area of Karamay oil field, Junggar basin, northwest China[J].AAPG Bulletin, 2005, 89(4):529-545.
[12] 邹才能, 侯连华, 陶士振, 等.新疆北部石炭系大型火山岩风化体结构与地层油气成藏机制[J].中国科学:地球科学, 2011, 41(11):1613-1626.
Zou Caineng, Hou Lianhua, Tao Shizhen, et al.Hydrocarbon accumulation mechanism and structure of large-scale volcanic weathering crust of the Carboniferous in northern Xinjiang, China[J].Science China:Earth Sciences, 2011, 55(2):221-235.
[13] 毛翔, 李江海, 张华添, 等.准噶尔盆地及其周缘地区晚古生代火山机构分布与发育环境分析[J].岩石学报, 2012, 28(8):2381-2391.
Mao Xiang, Li Jianghai, Zhang Huatian, et al.Study on the distribution and developmental environment of the Late Paleozoic volcanoes in Junggar Basin and its adjacent areas[J].Acta Petrologica Sinica, 2012, 28(8):2381-2391.
[14] Folk R L, Andrews P B, Lewis D W.Detrital sedimentary rock classification and nomenclature for use in New Zealand[J].New Zealand Journal of Geology and Geophysics, 1970, 13(4):937-968.
[15] Moncure G K, Surdam R C, McKague H L.Zeolite diagenesis below Pahute Mesa, Nevada Test Site[J].Clays and Clay Minerals, 1981, 29(5):385-396.
[16] 张丽媛, 纪友亮, 刘立, 等.火山碎屑岩储层异常高孔隙成因—以南贝尔凹陷东次凹北洼槽为例[J].石油学报, 2012, 33(5):814-821.
Zhang Liyuan, Ji Youliang, Liu Li, et al.Origin of anomalously high porosity in pyroclastic reservoirs:a case study on the northern region of the east sub-sag in Nanbeier sag[J].Acta Petrolei Sinica, 2012, 33(5):814-821.
[17] Hay R L.Geologic occurrence of zeolites[M]//Sand L B, Mumpton F A.Natural Zeolites:Occurrence, Properties, Use.New York:Pergamon Press, 1987:135-143.
[18] Orajaka I P.Behaviour of uranium during the formation and diagenetic alteration of silicic volcanoclastic sediments-a critical review[J].Uranium, 1987, 4(1):1-23.
[19] Mohamed B B, Bertrand F, Benoit M.Diagenetic albitization of K-feldspar and plagioclasein sandstone reservoirs:thermodynamic and kinetic modeling[J].Journal Sedimentary Research, 1993, 63(6):1100-1109.
[20] Land L S.Frio sandstone diagenesis, Texas Gulf Coast:a regional isotopic study[G].Clastic Diagenesis:AAPG Memoir 37, 1984:47-62.
[21] Schnaid F, Prietto P D M, Consoli N C.Characterization of cemented sand in triaxial compression[J].Journal of Geotechnical and Geoenvironmental Engineering, 2001, 127(10):857-868.
[22] Saidi F, Bernabe Y, Reuschle T.The mechanical behaviour of synthetic, poorly consolidated granular rock under uniaxial compression[J].Tectonophysics, 2003, 370(1):105-120.
[23] Spinelli G A, Mozley P S, Tobin H J, et al.Diagenesis, sediment strength, and pore collapse in sediment approaching the Nankai Trough subduction zone[J].Geological Society of America Bulletin, 2007, 119(3/4):377-390.
[24] Hurst A, Nadeau H P.Clay microporosity in reservoir sandstones:an application of quantitative electron microscopy in petrophysical evaluation[J].AAPG Bulletin, 1995, 79(4):563-573.
[25] Iijima A.Zeolites in petroleum and natural gas reservoirs[M]//Bish D L, Ming D W.Natural Zeolites:Occurrence, Properties, Applications.Washington:Mineralogical Society America, 2001:47-402.
[26] Galloway W E.Deposition and diagenetic alteration of sandstone in Northeast Pacific arc-related basins:implications for graywacke genesis[J].Geological Society America Bulletin, 1974, 85(3):379-390.
[27] Kaley M E, Hanson R F.Laumontite and leonhardite cement in Miocene sandstone from a well in San Joaquin Valley, California[J].American Mineralogist, 1955, 40:923-925.
[28] Yagi M.Regional metamorphism and hydrothermal alteration related to Miocene submarine volcanism ("green tuff") in the Yurihara oil and gas field, northwest Honshu island, Japan[J].The Island Arc, 1994, 2(4):240-261.
[29] 陈国俊, 吕成福, 王琪, 等.珠江口盆地深水区白云凹陷储层孔隙特征及影响因素[J].石油学报, 2010, 31(4):566-572.
Chen Guojun, Lü Chengfu, Wang Qi, et al.Characteristics of pore evolution and its controlling factors of Baiyun Sag in deepwater area of Pearl River Mouth Basin[J].Acta Petrolei Sinica, 2010, 31(4):566-572.
[30] Christidis G E.Formation and growth of smectites in bentonites:a case study from Kimolos Island, Aegean, Greece[J].Clays and Clay Minerals, 2001, 49(3):204-215. |