用户名: 密码: 验证码:
障壁碳酸盐岩台地类型与演化
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
论文在调研大量国内外文献的基础上,依托中国四川盆地、塔里木盆地、鄂尔多斯盆地以及中国南方海相碳酸盐岩研究成果,创新提出了基于“障壁条件、古地理条件和坡度”三要素的障壁碳酸盐岩台地成因分类,将台地划分为两大类8种类型,即缓坡型障壁台地、陡坡型障壁台地、缓坡型障壁孤立台地、陡坡型障壁孤立台地、缓坡型无障壁台地、陡坡型无障壁台地、缓坡型无障壁孤立台地、陡坡型无障壁孤立台地,同时总结了每一种台地的基本特征,建立了相应的沉积模式和储层发育与分布模式。揭示了碳酸盐岩台地演化与宇宙万物演化一样,通常经历形成、鼎盛和衰亡三个阶段,这三个阶段与构造伸展沉降期、构造稳定期和构造抬升期一致,总的呈两种演化趋势:一种是由无障壁台地向障壁台地演化,最后因抬升暴露而终止;另一种是由无障壁台地向障壁台地演化,最后因快速沉降,台地被淹没而结束。论文最后以四川盆地长兴组潮湿气候陡坡障壁台地、飞仙关组干旱气候陡坡障壁台地和嘉陵江—雷口坡组干旱气候陡坡障壁台地为例,详细解剖了三种障壁台地的岩相古地理特征和储层分布规律,指出有利的勘探方向。总之,论文既有基础理论的创新又有实际应用效果,具有良好的学术价值和实用价值。
Based on carbonate research results in Sichuan Basin, Tarim Basin, Ordos Basin and many literatures at home and abroad, the paper innovatively put forward a kind of genetic classification in carbonate platform which included three factors(barrier conditions, paleogeographic conditions and gradient).In this paper, platform was divided into two broad categories and eight sub-types, they are Barrier platform with gentle slope, Barrier platform with steep slope, Barrier isolation platform with gentle slope, Barrier isolation platform with steep slope, No barrier platform with gentle slope, No barrier platform with steep slope, No barrier isolation platform with gentle slope, No barrier isolation platform with steep slope. We summarized the basic characteristics of each kind of platform and established corresponding depositional mode, reservoir development and distribution pattern.
     We believe that evolution of carbonate platform just like the evolution of the universe, they Usually have three stages(formation, heyday and perish).these three stages are in accordance with tectonic stretch and subsidence, tectonic stable period and tectonic uplift period. There are two kinds of evolutionary trends:One is from No barrier platform evolved into Barrier platform, finally stopped due to uplift the exposure; The other is from No barrier platform evolved into Barrier platform, then platform was submerged because of rapid subsidence. The paper took Steep slope barrier platform with humid climate of Changxing Formation, Steep slope barrier platform with arid climate of Feixianguan Formation, Steep slope barrier platform with arid climate of Jialingjiang Formation and Leikoupo Formation in Sichuan basin as examples to detailedly dissected lithofacies paleographic characteristics and reservoir distribution rules of these three kinds of barrier platforms. The paper also pointed out advantageous exploration direction of three kinds of barrier platforms. Anyway the paper has innovation in Basic theory, actual application effect, academic and practical value.
引文
[I]Wilson, J. L Carbonate facies in geologic history [M].New York: Springer-Verlag,1975:471.
    [2]Read, J. F. Carbonate platform facies models[J].AAPG Bulletin,1985, 69(21):1-21.
    [3]Tucker M. E, Wright V. P, Dickson J. A. D. Carbonate sedimentology[M]. Blackwell Sci. Publ, Oxford, United Kingdom,1990:1-482.
    [4]顾家裕,马锋、季丽丹.碳酸盐岩台地类型、特征及主控因素.古地理学报,2009,11(1):21-27
    [5]郭庆新,周进高,寿建峰,等.障壁岛及其后缘碳酸盐岩储层的成因模式与预测.海相油气地质,2008,13(1):1-8.
    [6]周进高,张帆,邓红婴,等.鄂尔多斯盆地下奥陶统马家沟组障壁渴湖沉积相模式及有利储层分布规律[J].沉积学报,2011,2(15):61-70.
    [7]Tucker, M. E. Shallow-Marine carbonate facies and facies model[J]. in Brenchley, P, Williams, B. P. J. (eds):Sedimentology, recent development and applied aspects, Oxford (Blackwall),1985,18 (1):147-169.
    [8]Folk, R. L. Practical prtrographic classification of limestone[J]. AAPG,1959,43 (1):1-38.
    [9]Irwin M. L.General theory of epeiric clear water sedimentation[J]. Amer. Assoc. Petroleum Geologists Bull,1965,49:445-459.
    [10]Ahr, W. M. The carbonate ramp:an alternaive to the shelf model[J]. Transact. Gulf Coast Ass. Geol. Soc,1973,23:221-225.
    [11]Burchette, Wright.Carbonate ramp depositional systems[J]. Sed. Geol,1992,79:3-57.
    [12]James, Clarke. Cool water carbonates[J]. Soc. Econ. Paleont. Min. Spec. Publ,1997,56:1-20.
    [13]Erik Flugel. Microfacies of Carbonate Rocks[M]. Springer-Verlag Berlin Heidelberg,2004:1-695.
    [14]周进高,郭庆新,沈安江,等.四川盆地北部孤立台地边缘飞仙关组鲕滩储层特征及成因.海相油气地质,2012,17(2):57-62.
    [15]王一刚,文应初,洪海涛,等.四川盆地开江—梁平海槽内发现大隆组[J].天然气工业,2006,26(9):32-36.
    [16]王一刚,文应初,洪海涛,等.四川盆地及邻区上二叠统—下三叠统海槽的 深水沉积特征[J].石油与天然气地质,2006,27(5):702-714.
    [17]王一刚,文应初,洪海涛,等.四川盆地北部晚二叠世—早三叠世碳酸盐岩斜坡相带沉积特征[J].古地理学报,2009,11(2):143-156.
    [18]王兴志,张帆,马青,等.四川盆地东部晚二叠世—早三叠世飞仙关期礁滩特征与海平面变化.沉积学报,2002,20(2):249-254.
    [19]王一刚,文应初,张帆,等.川东地区上二叠统长兴组生物礁分布规律[J].天然气工业,1998,18(6):10-15.
    [20]张建勇,周进高,郝毅,等.四川盆地环开江—梁平海槽长兴组—飞仙关组沉积模式[J].海相油气地质,2011,16(3):7-15.
    [21]张继庆,李汝宁,官举铭,等.四川盆地及邻区生物礁[M].四川科学技术出版社,1990.(2):147-154.
    [22]范嘉松,吴亚生.川东二叠纪生物礁的再认识[J].石油与天然气地质,2002,23(1):12-18.
    [23]王生海,强子同.四川华蓥山涧水沟上二叠统生物礁[J].石油与天然气地质,1992,12(2):147-154.
    [24]吴熙纯,刘效曾,杨仲伦,等.川东上二叠统长兴组生物礁控储层的形成[J].石油与天然气地质,1990,11(3):283-296.
    [25]范嘉松,郭丽.川东上二叠统礁相及其储集层特征[J].海相油气地质,2000,5(2):152-152.
    [26]雷卞军,强子同,陈季高,等.川东上二叠统生物礁成岩作用与孔隙演化[J].石油与天然气地质,1991,12(4):364-375.
    [27]雷卞军,强子同.川东及邻区上二叠统生物礁的白云岩化[J].地质论评,1994,40(6):534-543.
    [28]强子同,文应初,雷卞军,等.川东鄂西上二叠统生物礁白云石化岩石学和地球化学[J].地球化学,1992,12(2):158-165.
    [29]冉隆辉,陈更生,徐仁芬.中国海相油气田勘探实例(之一)-四川盆地罗家寨大型气田的发现和探明[J].海相油气地质,2005,10(1):43-47.
    [30]马永生.中国海相油气田勘探实例(之六)-四川盆地普光大型气田的发现与勘探[J].海相油气地质,2005,10(1):43-47.
    [31]郝毅,周进高,张建勇,等,四川盆地鱼洞梁白云岩储层特征及控制因素[J].西南石油大学学报(自然科学版),2011,11(6):25-30.
    [32]苏立萍,罗平,罗忠,等.川东北飞仙关组鲕粒滩储层特征研究[J].天然气工业,2005,25(6):14-17.
    [33]王一刚,文应初,洪海涛,等.四川盆地三叠系飞仙关组气藏储层成岩作用研究拾零[J].沉积学报,2007,25(6):831-839.
    [34]魏国齐,杨威,张林,等,川东北飞仙关组鲕滩储层白云石化成因模式[J].天然气地球科学,2005,16(2):162-166.
    [35]陈更生,曾伟,杨雨,等.川东北部飞仙关组白云石化成因探讨[J].天然气工业,2005,25(4)40-41.
    [36]郑荣才,耿威,郑超,等.川东北地区飞仙关组优质白云岩储层的成因[J].石油学报,2008,29(6)815-821.
    [37]黄思静,Hairuo QING,胡作维,等.四川盆地东北部三叠系飞仙关组碳酸盐岩成岩作用和白云岩成因的研究现状和存在问题[J].地球科学进展,2007,22(5):495-503.
    [38]黄思静,Hairuo QING,裴昌蓉,等.川东三叠系飞仙关组白云岩锶含量、锶同位素组成与白云石化流体[J].岩石学报,2006,22(8):2123—2132.
    [39]高梅生,郑荣才,文华国,等.川东北下三叠统飞仙关组白云岩成因—来自岩石结构的证据[J].成都理工大学学报:自然科学版,2007,34(3):297—304.
    [40]穆曙光,周茂,华永川.川东北地区下三叠统飞仙关组白云岩成因类型[J].天然气工业,1994,14(3):23—27.
    [41]张建勇,周进高,潘立银,等.川东北地区孤立台地飞仙关组优质储层形成主控因素——大气淡水淋滤及渗透回流白云石化[J].天然气地球科学,2013,24(1):9-18.
    [42]曾伟,黄先平,杨雨,等.川东北地区飞仙关组储层中的埋藏溶蚀作用[J].天然气工业,2006,26(11):40-41.
    [43]杨晓萍,赵文智,曹宏,等.川东北三叠系飞仙关组鲕滩气藏有利储集层的形成与分布[J].石油勘探与开发,2006,33(1):17-21.
    [44]潘立银,刘占国,李昌,等.四川盆地东部下三叠统飞仙关组白云岩化作用及其与储集层发育的关系[J].古地理学报,2012,14(2):176-187.
    [45]王一刚,刘划一,文应初,等.川东北飞仙关组鲕滩储层分布规律、勘探方法与远景预测[J].天然气工业,2002,增刊:14-18.
    [46]杨雨,王一刚,文应初,等.川东飞仙关组沉积相与鲕滩气藏的分布[J].天然气勘探与开发,2001,24(3):18-21.
    [47]四川省地质矿产局.四川省区域地质志[M].北京:地质出版社,1991.
    [48]郭正吾,邓康龄,韩永辉,等.四川盆地形成与演化[M].北京:地质出版社,1996.
    [49]车自成,刘良,罗金海,等.四川盆地形成与演化[M].北京:科学出版社,2002.
    [50]冯增昭.沉积岩石学[M].北京:石油工业出版社,1993.
    [51]崔树德,魏凌琛.早、中三叠世四川盐地古地理概况及与油气关系探讨[G]//岩相古地理文集(2).北京:地质出版社,1986.
    [52]朱洪发,刘翠章,林傅律.四川盆地中下三叠统成盐古地理景观、成盐机理及钾盐预测[G]//岩相古地理文集(4).北京:地质出版社,1988.
    [53]吴应林,袁敬阆.上扬子地区三叠纪蒸发岩的成因和相模式[M].北京:地质出版社,1985.
    [54]陈莉琼,沈昭国,侯方浩,等.四川盆地三叠纪蒸发岩盆地形成环境及白云岩储层[J].石油实验地质,2010,(4):334-340.
    [55]沈安江,周进高,辛勇光,等.四川盆地雷口坡组白云岩储层类型及成因[J].海相油气地质,2008,13(4):19-28.
    [56]李晓清,汪泽成,张兴为,等.四川盆地古隆起特征及对天然气的控制作用[J].石油与天然气地质,2001,22(4):347-351.
    [57]陈洪德,侯明才,刘文均,等.海西—印支期中国南方的盆地演化与层序格架[J].成都理工大学学报(自然科学版),2004,31(6):629-635.
    [58]林耀庭,姚有成,康正华,等.四川宣达盐盆富钾富矿卤水地球化学特征及资源意义研究[J].盐湖研究,2004,12(1):8-18.
    [59]朱井泉.四川华蓥山三叠系含膏盐段的碳氧同位素特征及其意义[J].岩石学报,1990,11(4):67-74.
    [60]张廷山,陈晓慧,姜照勇,等.泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J].沉积学报,2008,26(4):583-591.
    [61]韩克遒.川东开江古隆起大中型气田的形成及勘探目标[J].天然气工业,1995,15(4):1-4.
    [62]林良彪,陈洪德,张长俊,等.四川盐地西北部中三叠世雷口坡期岩相古地理[J].沉积与特提斯地质,2007,27(3):52-58.
    [63]侯方浩,方少仙.四川盆地川西地区中三叠统雷口坡组岩相古地理及储集条件研究[R].四川石油管理局川中矿区,1993.
    [64]李伦俊,王新建.四川盆地中、下三叠统沉积相及储集层研究报告[R].四川石油管理局研究院,1984.
    [65]曾学思,田端孝,崔德树,等.四川盆地西部中三迭统雷口坡组岩相及油气水关系的探讨[R].四川石油管理局研究院,1978.
    [66]周进高,辛勇光,谷明峰,等,四川盆地中三叠统雷口坡组天然气勘探方向[J].天然气工业,2010,30(12):16-19.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700