阿克库勒凸起东河砂岩的沉积相与层序地层

doi:10.11743/ogg20050621

摘要/Abstract

摘要：

阿克库勒地区东河砂岩包括了含泥砾砂岩、分选好的中-细粒砂岩、粉砂岩及泥岩,是一个具有完整海侵-海退旋回的标准层序,顶、底分别为两个不整合面所限,为Ⅰ型层序边界。东河砂岩自下而上明显地分为低位体系域、海侵体系域与高位体系域。由于低位体系域是陆上河流的充填沉积,因此,盆地内低位体系域不发育,分布局限。海侵体系域主要为受潮汐控制的滨岸沉积,由一系列向上变浅和变细的副层序堆积成退积的副层序组,副层序由下部的潮下砂坝向上逐渐变化为潮间砂坪、砂泥混合坪及泥坪。高位体系域主要分布于东河砂岩的上段,由于东河砂岩的不断沉积,在达到最大海泛面之后,滨岸带海水循环畅通,形成了以波浪作用为主的浪控滨岸沉积体系,主要是以分选好的灰白色中-细粒砂岩为特征,构成了特色十分鲜明的“东河砂岩”。

关键词: 沉积相, 潮控滨岸, 浪控滨岸, 层序地层, 东河砂岩, 塔里木盆地

Abstract:

Donghe sandstone in Akekule,composed of mud-pebbly sandstone,well sorted(medium-to)fine-grained sandstones,siltstone and mudstone,is a normal sequence with a complete transgressive-regressive cycle,the top and bottom of which are defined by unconformities,i.e.,type Ⅰsequence boundaries.Donghe sandstone can evidently be divided,from bottom to top,into lowstand system tract,transgressive system tract and highstand system tract.As the lowstand system tract is subaerial fluvial deposit,it is underdeveloped in the basin with limited distribution.The transgressive system tract is mainly composed of shore deposit controlled by tide.A series of shallowing and fining upward parasequences constitute the retrograding parasequence group.The parasequences gradually change upward from subtidal sandbar in the lower part to intertidal sand flat,mixed sand and mud flat,and mud flat.The highstand system tract is mainly distributed in the upper Donghe sandstone.Duing the continuous deposition of Donghe sandstone, the inshore sea water circulated smoothly and(unimpededly)after the largest marine flooding surface was reached,leading to the formation of wave-controlled shore deposition system with wave action as the main geologic agent,which is mainly characterized by grayish white(medium-to)fine-grained sandstone. They constitute the characteristic "Donghe sandstone".

Key words: sedimentary facies, tide-controlled shore, wave controlled shore, sequence stratigraphy, Donghe sandstone, Tarim basin

中图分类号:

TE112.2

郭建华,朱美衡,刘辰生,等. 阿克库勒凸起东河砂岩的沉积相与层序地层[J]. 石油与天然气地质, 2005, 26(6): 808-815. doi: 10.11743/ogg20050621 Guo Jianhua,Zhu Meiheng,Liu Chensheng,et al. Sedimentary facies and sequence stratigraphy of Donghe Sandstone in Akekule Uplift[J]. Oil & Gas Geology, 2005, 26(6): 808-815. doi: 10.11743/ogg20050621

参考文献

[1] 郭建华,曾允孚,翟永红,等.塔中地区石炭系东河砂岩层序地层研究[J].沉积学报,1996,14(2):56～65Guo Jianhua,Zeng Yunfu,Zhai Yonghong,et al.Sequence stratigraphy of Carboniferous Donghe sandstone in Tazhong area,Ta-rim basin[J].Acta Sedimentologica Sinica,1996,14(2):56-65
[2] 杨松岭,高增海,赵秀岐.塔里木盆地东河砂岩层序特征与分布规律[J].新疆石油地质,2002,23(1):35～37Yang Songling,Gao Zenghai,Zhao Xiuqi.The characteristic and distribution of Donghe sandstone sequences in Tarim basin[J].Xinjiang Petroleum Geology,2002,23(1):35-37
[3] 顾家裕.塔里木盆地石炭系东河砂岩沉积环境分析及储层研究[J].地质学报,1996,70(2):153～161Gu Jiayu.Sedimentary environment and reservoir characters of the Carboniferous Donghe sandstone in the Tarim basin[J].Acta Geologica Sinica,1996,70(2):153-161
[4] 朱筱敏,张强,赵澄林,等.塔里木中部地区东河砂岩段沉积特征和沉积环境演变[J].地质科学,2004,39(1):27～35Zhu Xiaomin,Zhang Qiang,Zhao Chenglin,et al.Sedimentary faccies and environmental change of the Donghe sandstone in central Tarim[J].Chinese Journal of Geology,2004,39(1):27-35
[5] 王招明,王清华,孙丽霞,等.东河砂岩钙结成岩作用的主要特征[J].地质科学,2004,39(4):517～522Wang Zhaoming,Wang Qinghua,Sun Lixia,et al.Main features of calcic-diagenesis in the Donghe sandstone[J].Chinese Journal of Geology,2004,39(4):517-522
[6] 钟大康,朱筱敏,周新源,等.塔里木中部泥盆系东河砂岩成岩作用与储集性能控制因素[J].古地理学报,2003,5(3):378～390Zhong Dakang,Zhu Xiaomin,Zhou Xinyuan,et al.Diagenesis and controlling factors of reservoir quality of Devonian Donghe sandstone[J].Journal of Palaeogeography,2003,5(3):378-390
[7] 孙玉善,杨帆.再论东河砂岩孔隙成因--以塔中地区为例[J].沉积学报,1999,17(增刊):609～705Sun Yushan,Yang Fan.Rediscussion on pore genesis of Donghe sandstone-an example from Tazhong area[J].Acta Sedimentologica Sinica,1999,17(supp):609-705
[8] 翟永红,郭建华,刘生国.塔中地区石炭系深埋藏优质碎屑岩储层成因分析[J].矿物岩石,1996,16(2):55～61Zhai Yonghong,Guo Jianhua,Liu Shengguo.Study on the origin of quality clastic rock reservoir in Carboniferous from Tazhong area[J].Journal of Mineralogy and Petrology,1996,16(2):55-61
[9] 郭建华,石媛媛,刘辰生.阿克库勒凸起西缘东河砂岩储集物性非均质性研究[J].沉积学报,2005,23(3):406～411Guo Jianhua,Shi Yuanyuan,Liu Chensheng.Non-homogeneity of Donghe sandstone on the western margin of Akekule uplift[J].Acta Sedimentologica Sinica,2005,23(3):406-411
[10] 何登发,贾承造,李德生,等.塔里木多旋回叠合盆地的形成与演化[J].石油与天然气地质,2005,26(1):64～77He Dengfa,Jia Chengzao,Li Desheng,et al.Formation and evolution of polycyclic superimposed Tarim basin[J].Oil & Gas Geology,2005,26(1):64-77
[11] 贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997Jia Chengzao.The tectonic characters and oil & gas in Tarim basin of China[M].Beijing:Petroleum Industry Press,1997
[12] 朱怀诚,罗辉,王启飞,等.论塔里木盆地"东河砂岩"的地质时代[J].地层学杂志,2002,26(3):197～201Zhu Huaicheng,Luo Hui,Wang Qifei,et al.The age of the Donghe sandstone in the Tarim basin[J].Journal of Stratigraphy,2002,26(3):197-201
[13] 朱怀诚.塔里木盆地草2井东河砂岩段孢子组合的时代[J].微体古生物学报,1998,15(4):395～403Zhu Huaicheng.On the age of spore assembleage from Donghe sandstone in well Cao-2 of north Tarim basin[J].Acta Micropalaeontologica Sinica,1998,15(4):395-403
[14] 刘静江.塔中45井泥盆纪鱼类化石的发现及东河砂岩的时代[J].新疆石油地质,1998,19(2):180～182Liu Jingjiang.Discovery of Devonian fish fossil in well Tazhong 45 and age of Donghe sandstone[J].Xinjiang Petroleum Geology,1998,19(2):180-182
[15] 郭建华,曾允孚,翟永红,等.新疆塔中石炭系层序地层学研究--一个克拉通内坳陷盆地的层序地层框架模式[J].地质学报,1996,70(4):361～373Guo Jianhua,Zeng Yunfu,Zhai Yonghong,et al.On the Carbo-niferous sequence stratigraphy in the Tazhong area,Xinjiang:a model of the sequence stratigraphy framework of intra-cratonic depressional basin[J].Acta Geologica Sinica,1996,70(4):361-373
[16] 郭建华,王明艳,蒋小琼,等.塔里木盆地塔中、满西地区石炭系层序地层[J].中南工业大学学报,2004,35(1):122～128Guo Jianhua,Wang Mingyan,Jiang Xiaoqiong,et al.Sequence stratigraphy of the Carboniferous in Tazhong and Manxi areas of Tarim basin[J].Journal of South-Central University(Natural Science),2004,35(1):122-128
[17] Posamentier M W,Allen G P.Siliciclastic sequence stratigraphic patterns in foreland ramp-type basins[J].Geology,1993,21:455-458
[18] Alvarez L W,Alvarez W,Asaro F,et al.Extraterrestrial cause for the Cretaceous-Tertiary extinction[J].Science,1980,208:1 095-1 107
[19] 周瑶琪,陆永潮,李思田,等.间断面缺失时间的计算问题[J].地质学报,1997,71(1):7～17Zhou Yaoqi,Lu Yongchao,Li Sitian,et al.The missing time calculation of the hiatus surface[J].Acta Geologica Sinica,1997,71(1):7-17
[20] 周瑶琪,柴之芳,毛雪瑛,等.混合成因模式--中国南方二叠三叠系地层元素地球化学及其启示[J].地质论评,1991,37(1):51～63Zhou Yaoqi,Chai Zhifang,Mao Xueying,et al.A mixing mo-del-the element geochemistry of Permian-Triassic boundaries in South China and its implication[J].Geological Review,1991,37(1):51-63
[21] van Wagoner J C,Mitchum R M,Campion K M,et al.Siliciclastic sequence stratigraphy in well logs,cores and outcrops concepts for high-resolution correlation of time and facies[J].AAPG Me-thods in Exploration Series,1990,(7):1-55
[22] 郭建华,刘生国,翟永红.塔中地区石炭系碎屑岩岩石学特征与物源分析[J].江汉石油学院学报,1995,17(3):1～7Guo Jianhua,Liu Shengguo,Zhai Yonghong.Carboniferous siliciclastic rocks in Tazhong area:their petrology features and material sources[J].Journal of Jianghan Petroleum Institute,1995,17(4):1-7
[23] 郭建华,吴智勇,翟永红.塔中四井区东河砂岩段中的河口湾沉积[J].江汉石油学院学报,1995,17(4):5～11Guo Jianhua,Wu Zhiyong,Zhai Yonghong.Estuary sedimentary system of Carboniferous Donghe sandstone in Tazhong 4 well area[J].Journal of Jianghan Petroleum Institute,1995,17(4):5-11