黔桂地区泥盆系层序地层格架及相对海平面变化

梅冥相; 高金汉; 李东海; 孟庆芬; 易定红

黔桂地区泥盆系层序地层格架及相对海平面变化

中国地质大学地球科学与资源学院北京 100083

基金项目: 中国石化集团科技工程项目(NPJ-10019)的成果之一

详细信息

作者简介:
梅冥相,男,1965年出生,教授,理学博士,沉积学与地层学

中图分类号: P539.2;P534.44

计量

文章访问数: 662
HTML全文浏览量: 7
PDF下载量: 740
被引次数: 0

Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

Faculty of Earth Sciences and Resources, China University of Geosciences, Beijing 100083

摘要

摘要: 志留纪末期的加里东运动,使黔桂地区的古地理格局发生了重大变化,早古生代的滇黔桂古陆演变为晚古生代的滇黔桂海。泥盆纪初期,海水由南而北逐渐海侵超覆,在泥盆系的底部形成一套海侵碎屑岩系地层;早泥盆世晚期的大规模海侵事件造成了明显的相分异,在习称的滇黔桂盆地中发育了若干孤立碳酸盐台地,这种“台—盆—丘—槽”的格局一直延续到晚泥盆世早期;而泥盆纪末期的紫云运动所造成的地壳抬升,又使晚泥盆世地层产生海退尖灭。因此,该地区的泥盆系构成一个二级构造层序,其中包含13个三级沉积层序。在前人大量生物地层学研究的基础上,追索和对比不同沉积背景中的三级沉积层序的相序组构特征以及由其所代表的相对海平面变化,即可建立黔桂地区泥盆系的层序地层格架。层序地层格架较为充分地表现出三级沉积层序的两大特征——空间上相序的有序性和时间上环境变化的同步性,同时也明显地显示出地层记录中的两种相变面和两种穿时性。
- 层序地层格架 /
- 泥盆系 /
- 黔桂地区
Abstract: There is a great change of paleogeography setting resulted from the Caledonian orogeny at the end of Silurian in Guizhou and Guangxi area in south China, the Dianqiangui oldland in early Paleozoic evolved as the Dianqiangui sea in late Plaeozoic. In the initial stage of Devonian Period, seawater is onlaped gradually from the south to the north caused by transgression, so the bottom part of Devonian system is constituted by a set of transgressive clastic sedimentary rock. The great scale transgressive event at the end of the early Epoch of Devonian forms evident differentiation of depositional facies in Guizhou and Guangxi province, a lot of isolated carbonate platforms are developed in Dianqiangui Basin, the special paleogeographic setting marked by "platforms-basins-hills-trough" is formed and lasted to the early stage of the late Epoch of Devonian. The strata of the upper Epoch of Devonian become regressive thin out from paleosea to oldland resulted from the Ziyun epeirogeny that took place in the transitional period from Devonian Period to Carboniferous Period. On the basis of the study on the evolutional natures of sediments in time and the distribution characters of sedimentary facies in space, 13 third-order sedimentary sequences are discerned in Devonian strata in Guizhou and Guangxi province, which could be grouped into one second-order tectonic sequence. In terms of the correlation on biostratigraphy, the sea-level changes delegated by third-order sequences with different architecture natures of facies-succession also could be correlative in research region, in the end, the framework of sequence stratigraphy could be constructed. Many characters such as two elementary natures of third-order sequences——“the regularity of facies-succession in space and the synchronism of the changes of sedimentary environment in time”, two kinds of diachronism that are relative to two types of facies-changing surfaces——“the diachronism of facies-changing surfaces caused by static facies-changing surface and the diachronism of punctuated surfaces formed by dynamic facies-changing surfaces" in strtigraphic records, are clearly demonstrated in the framework of sequence stratigraphy.
- the framework of sequence stratigraphy /
- Devonian system /
- Guizhou and Guangxi area in south China

HTML全文

参考文献(20)

[1]	侯鸿飞,曹宣铎,王士涛,鲜思远,王金星.中国地层典(泥盆系)[M].北京:地质出版社,2000.1～118[Hou Hongfei,Cao Xuanduo, Wang Shitao, Xian Siyuan, Wang Jinxing. Chinese stratigraphic lexicon ( Devonian system)[M]. Beijing: Geological Publishing House,2000.1 ～ 118
[2]	赵自强,丁启秀主编.中南区区域地层[M].武汉:中国地质大学出版社,1996.71～123[Zhao Ziqiang,Ding Qixiu.The regional stratigraphy in central and south part of China[M]. Wuhan: China U-niversity of Geosienes Press,1996 71～123]
[3]	董卫平主编.贵州省岩石地层[M].武汉:中国地质大学出版社,1997. 143 ～ 220 [Dong Weiping. Lithostratigraphy in Guizhou [M].Wuhan: China University of Geosciences Press, 1997. 143～220]
[4]	殷保安主编.广西状族自治区岩石地层[M].武汉:中国地质大学出版社,1997 52～191[Yin Baoan.Lithostratigraphy in Guangxi[M].Wuhan:China University of Geosciences Press,1997.52～191]
[5]	曾允乎,张锦泉,刘文均等.中国南方泥盆纪岩相古地理与成矿作用[M].北京:地质出版社,1994.1～120[Zen Yunfu,Zhang Jinquan, Liu Wenjun, Zhou Huailin, Chen Hongde. Devonian lithofacies paleogeography and mineralization in south China[M]. Beijing: Geological Publishing House, 1994. 1～120]
[6]	吴诒,周怀玲,蒋廷操等.广西泥盆纪沉积相古地理及矿产[M].南宁:广西人民出版社,1987.1～256[Wu Yi,Zhou Huailing,Jiang Tingchao Fang Daonian, Huang Wusheng. The sedimentary facies paleogeography and relatively mineral deposits of Devonian in Guangxi[M].Nanning: Guangxi Peoples Publishing Hoase, 1987.1 ～256]
[7]	钟铿,吴诒,殷保安等.广西的泥盆系[M].武汉:中国地质大学出版社,1992.1～370[Zhong Keng,Wu Yi,YinBaoan,et al.Devonian systen of Guangxi[M]. Wuhan: China University of Geosciences Press, 1992. 1～370]
[8]	邝网敦,赵明特,陶业斌编著广西六景泥盆系剖面[M].武汉:中国地质大学出版社,1989.1～155[Kuang Guodun,Zhao Mingte,Tao Yebin. The standard Devonian section of China: Liujing section of Guangxi[M]. Wuhan: China University of Geosciences Press, 1989.1～154]
[9]	许效松,牟传龙,林明著.露头层序地层与华南泥盆纪古地理[M].成都:成都科技大学出版社,1993.1～288[Xu Xiaosong,Mou Chuanlong, Lin Ming. The outcrop sequence stratigraphy of Devonian and palcogeography in south-China[M]. Chengdu: Chengdu University of Sciencs and Technology Press, 1993. 1 ～288]
[10]	吴诒,龚一鸣,杜远生.华南泥盆纪层序地层及海平面变化[M].武汉:中国地质大学出版社,1997.1～98[Wu Yi,Du Yuansheng,Gong Yiming. Devonian sequenoe stratigraphy and the relative sea-lev-el changes in South-China [M]. Wuban: China University of Geosciences Press, 1997. 1～98]
[11]	杨惠民,刘炳温,邓宗怀等.滇黔桂海相碳酸盐岩地区最佳油气保存单元的评价与选择[M].贵阳:贵州科技出版社,1999.4～63[Yang Huiming, Liu Binwen, Deng Zonghuai, et al. Value and Selection to the Best Gas-Oil Keeping Unite of Marine Carbonate Area in Yunnan, Guizhou and Guangxi[M]. Guiyang: Guizhou Science and Technology Press, 1999. 4 ～63]
[12]	梅冥相,马永生,戴少武等.南盘江盆地晚古生代盆地充填序列特征及生储盖组合划分[J].现代地质,2001,15(1):74～82[Mei Mingxiang, Ma Yongsheng, Dai Shaowu, et al. Late Paleozoic filling succession of the Dianqiangui Basin and the division of association of oilgenerating strata, reservoir, and capping bed[J]. Geosciences,2001,15(1), 74～82]
[13]	吴浩若.广西加里东运动构造古地理问题[J].古地理学报,2000,2(1): 70 ～ 76 [Wu Haoruo. A discussion on the tectonic paleogeography related to the Caledonian movement in Guangxi[J]. Journal of Paleogeography, 2000,2(1): 70～76]
[14]	陈旭,阮亦萍,AJ布科主编,中国古生代气候演变[M].北京:科学出版社,2001 40～53[Chen Xu,Ruan Yiping,A J Boucot.The climate evolution of Plaeozoic in China [M]. Beijing: Sciences Press, 2001, 40～53]
[15]	梅冥相,马永生.从旋回层序的特征论地层记录的两种相变面及两种穿时性[J].地层学杂志,2001,25(2):150～153[Mei Mingxiang, Ma Yongsheng. On two kinds of Facies-change surface and two kinds of diachronisa in stratigraphical records according to the natures of cyclic-sequences[J]. Journal of Stratigraphy, 2001,25(2): 150-153]
[16]	梅冥相.从地层记录的特征论岩石地层学的困惑[J].地层学杂志,1996,20(3):207～212[Mei Mingxiang.On the perplexity of lithostratigraphy according to the natures of stratigraphic records[J].Journal of Stratigraphy, 1996, 20(3): 207～212]
[17]	周希云.贵州泥盆纪几个地层问题的讨论[J].贵州地质,1992,9(4): 331～339[Zhou Xiyun. On discussion of the several problens on Devonian stratigraphy[J]. Guizhou Geology, 1992, 9 (4): 331 ～339]
[18]	Enos P , Wei Jiayong, Lehrmann D J. Death in Guizhou-Late Triassic dromning of the Yangtze carbonate platform[J]. Sedimentary Geology, 1998, 118:55～76
[19]	Johson J G, Klapper G. North American Midcontinent Devonian T-R cycles[J]. Oklahoma Geological Survey Bulletin, 1992,145: 127～135
[20]	Ross C A, Ross J R P. Late Paleozoic transgressive-regressive deposition[A]. In: Wilgus C K, ed. Sea-level Changes: an Integrated Aptoroach[C]. SEPM Spec Pub, 1988, 42:227～247

[1]	宋爽, 朱筱敏, 于福生, 葛家旺, 史亚会, 贺敬聪, 袁立忠, 刘军. 珠江口盆地长昌-鹤山凹陷古近系沉积-构造耦合关系 . 沉积学报, 2016, 34(2): 222-235. doi: 10.14027/j.cnki.cjxb.2016.02.002
[2]	. 梨树断陷营城组层序地层格架与沉积相特征 . 沉积学报, 2014, 32(3): 576-585.
[3]	刘畅, 张琴, 谢寅符, 乔李井宇, 孙杰夫, 梅啸寒. 厄瓜多尔Oriente盆地东北部区块白垩系层序地层格架及发育模式 . 沉积学报, 2014, 32(6): 1123-1131.
[4]	袁红旗. 海拉尔盆地查干诺尔凹陷下白垩统层序地层学研究 . 沉积学报, 2008, 26(2): 241-248.
[5]	张哲杜远生毛治超李瑞原小杰. 湘东南桂阳莲塘上泥盆系风暴岩特征及其古地理、古气候意义 . 沉积学报, 2008, 26(3): 369-375.
[6]	管红. 南堡凹陷东营组层序地层格架与沉积体系 . 沉积学报, 2008, 26(5): 730-736.
[7]	郭彦如刘化清李相博完颜容郑希民. 大型坳陷湖盆层序地层格架的研究方法体系 ———以鄂尔多斯盆地中生界延长组为例 . 沉积学报, 2008, 26(3): 384-391.
[8]	. 三级基准面旋回内三角洲砂体骨架模型的建立——以陕北安塞三角洲露头为例 . 沉积学报, 2006, 24(4): 540-548.
[9]	梁积伟. 鄂尔多斯盆地东北部山西组高分辨层序地层学研究 . 沉积学报, 2006, 24(2): 251-258.
[10]	方维萱, 张国伟, 胡瑞忠, 刘方杰. 秦岭造山带泥盆系热水沉积岩相应用研究及实例 . 沉积学报, 2001, 19(1): 48-54.
[11]	桑树勋, 李壮富, 范炳恒, 陈世悦. 层序地层格架与煤岩层对比——层序地层学在山西阳曲煤田普查勘探中的应用 . 沉积学报, 2001, 19(4): 556-562.
[12]	覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区泥盆系层序地层分析 . 沉积学报, 2000, 18(2): 172-179.
[13]	田景春, 陈洪德, 彭军, 覃建雄, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区下、中三叠统层序划分、对比及层序地层格架 . 沉积学报, 2000, 18(2): 198-204.
[14]	杜远生, 龚一鸣, 吴诒, 冯庆来, 刘本培. 黔桂地区泥盆纪层序地层和台内裂陷槽的形成演化 . 沉积学报, 1997, 15(4): 11-17.
[15]	王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境 . 沉积学报, 1995, 13(3): 13-22.
[16]	龚一鸣. 新疆北部泥盆系火山碎屑浊积岩层序结构特征及其地质意义 . 沉积学报, 1993, 11(2): 75-83.
[17]	杜远生, 赵锡文. 甘肃西成铅锌矿田泥盆纪吉维特—弗拉斯期沉积古地理及控矿意义 . 沉积学报, 1991, 9(3): 22-30.
[18]	刘文均. 湘南泥盆系碳酸盐岩中锶的分布特点及其环境意义 . 沉积学报, 1989, 7(2): 14-20.
[19]	高计元. 中国南方泥盆系瘤状灰岩的成因 . 沉积学报, 1988, 6(2): 77-86.
[20]	陈先沛, 高计元. 广西中部泥盆系的多金属-重晶石矿床和热水沉积作用 . 沉积学报, 1987, 5(3): 149-158.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 662
HTML全文浏览量: 7
PDF下载量: 740
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

黔桂地区泥盆系层序地层格架及相对海平面变化

作者简介:
梅冥相,男,1965年出生,教授,理学博士,沉积学与地层学

计量

Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

计量

目录

黔桂地区泥盆系层序地层格架及相对海平面变化

中国地质大学地球科学与资源学院北京 100083

作者简介:
梅冥相,男,1965年出生,教授,理学博士,沉积学与地层学

English Abstract

Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

Faculty of Earth Sciences and Resources, China University of Geosciences, Beijing 100083

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

黔桂地区泥盆系层序地层格架及相对海平面变化

作者简介: 梅冥相,男,1965年出生,教授,理学博士,沉积学与地层学

计量

出版历程

Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

计量

出版历程

目录

黔桂地区泥盆系层序地层格架及相对海平面变化

中国地质大学地球科学与资源学院 北京 100083

作者简介: 梅冥相,男,1965年出生,教授,理学博士,沉积学与地层学

English Abstract

Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

Faculty of Earth Sciences and Resources, China University of Geosciences, Beijing 100083

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
梅冥相,男,1965年出生,教授,理学博士,沉积学与地层学

中国地质大学地球科学与资源学院北京 100083

作者简介:
梅冥相,男,1965年出生,教授,理学博士,沉积学与地层学