THE TYPE OF QUATERNARY SEQUENCE IN THE EAST CHINA COASTAL PLAIN
-
摘要: 据渤海湾西岸、长江三角洲地区钻孔资料,确定在构造沉降背景下形成的中国东部沿海平原第四系见两类层序。超过0.10 Ma周期的大洪泛事件,分别发生在约2.60、0.8、0.5(?)和0.15 Ma前后,相当于层序地层的水进体系域,在天津北部平原系华北盆地北边缘山体周期性隆升,在长江一线是附近低山丘陵周期性隆升的表现,反映沿海平原环境变化对西部构造-气候旋回的响应。MIS5以来沿海出现受全球海面变化控制的3期10 ka级海侵,结合海域研究可以确定MIS1期间出现完整的海侵-海退层序,沿海平原10 ka开始的全新世沉积为高位体系域,7~10 ka基底泥炭作为最大海进面,在下切河谷内可见14C测年早于10 ka的泥炭。Abstract: Based on materials from the drilling holes in the west coast of Bohai Bay and the Yangtze River delta area, the present paper determined two types of sequence stratigraphy in the East China coastal plain formed under the tectonic subsidence setting. The great flooding events which had a cycle of over 0.10 Ma in the fluvial system and occurred at cir. 2.60 Ma, 0.8 Ma, 0.5 Ma (?) and 0.15 Ma respectively, could be correlated to the transgressive system tract(TST)in the sequence stratigraphy. These are related to the periodic uplifting of northern mountain in the North China basin in the north of Tianjin and to that of low mountain and hills along the Yangtze River, and all represent the response of environment in the coastal plain to the tecto-climatic cycles in West China. Since MIS5 three transgressions with 10 ka period controlled by global sea-level change occurred in East China coastal plain. Combining with research results in the sea region, it can be determined that a complete transgression-regression sequence appeared in MIS1 period; in the coastal plain the Holocene transgression bed formed since 10 ka is corresponding to the parasequence in the high-stand tract (HST). The basal peat dated 7~10 ka is the maximum flooding surface and the peat older than 10 ka in 14C age could be found at the incised valley.
-
Key words:
- sequence stratigraphy /
- type /
- Quaternary system /
- East China coastal plain
-
-
[1] Posamentier H W,Vall P R.Eustatic controls on clastic deposition Ⅱ:Sequence and systems tract models[C]//In:Wilgus C K, et al (eds.).Sea-Level Changes:An Integrated Approach.1988, SEPM Sp. Publ. 42:125-154.
[2] Van Wagoner J C, Mitchurn R M, Camplonm K M, et al.Siliciclastic sequence stratigraphy in well logs, cores and outcrops:Concepts for high resolution correlation of time and facies[J]. AAPG,1990, Methods in Exploration Series, 7:1-54.
[3] Holland K T, Elmore P A. A review of heterogeneous sediments in coastal environments[J]. Earth-Science Reviews, 2008, 89:116-134.
[4] 李从先,闵秋宝,孙和平.长江三角洲南翼全新世地层和海侵[J].科学通报,1986,46(21):1650-1653.
[LI Congxian, MIN Qiubao,SUN Heping. Holocene strata and transgression on the south side of Changjiang Delta[J]. Chinese Science Bulletin, 1986,46(21):1650-1653.]
[5] 李从先,陈刚.冰后期海岸层序的初步研究[J].海洋学报,1985,7(1):34-43.
[LI Congxian, CHEN Gang. Preliminary study on the sequence of post glacial period[J]. Acta Oceanologica Sinica, 1985,7(1):34-43.]
[6] 李从先,张桂甲.晚第四纪长江三角洲高分辨率层序地层学的初步研究[J].海洋地质与第四纪地质,1996,16(3):13-24.
[LI Congxian, ZHANG Guijia. A preliminary study on high resolution sequence stratigraphy of Late Quaternary in the Yangtze River delta area[J]. Marine Geology and Quaternary Geology, 1996, 16(3):13-24.]
[7] 李从先,汪品先.长江晚第四纪河口地层学研究[M].北京:科学出版社,1998:4-198.[LI Congxian, WANG Pinxian, et al. Late Quaternary Estuary Stratigraphy of the Changjiang (Yangtze) Delta[M]. Beijing:Science Press, 1998:4
-198.]
[8] 王强,李凤林.渤海湾西岸第四纪海陆变迁[J].海洋地质与第四纪地质,1983,3(4):83-89.
[WANG Qiang, LI Fenglin. The changes of marine-terregenous condition in the west coast of the Bohai Bay during Quaternary[J]. Marine Geology and Quaternary Geology, 1983,3(4):83-89.]
[9] 王强,李凤林,李玉德,等.对渤海西、南岸第四纪海侵命名的讨论[J].海洋学报,1986,8(1):71-81.
[WANG Qiang, LI Fenglin, LI Yude, et al. Discussion on the naming of Quaternary transgressions in west-southern coast plain of Bohai Sea[J]. Acta Oceanologica Sinica, 1987, 6(1):104-115.]
[10] 王强,李凤林,李玉德,等.十五万年来渤海西、南岸平原海岸线变迁[C]//见:赵松龄,苍树溪.中国海平面变化(IGCP200项中国工作组).北京:海洋出版社,1986:43-52.[WANG Qiang, LI Fenglin, LI Yude, et al. The change of shoreline in west-southern plain of the Bohai Sea since 150 ka[C]//In:ZHAO Songling,CANG Shuxi (eds.) Sea-Level Change in China (IGCP200
Project China National Working Group). Beijing:China Ocean Press, 1986:43-52.]
[11] 王强,田国强.中国东部晚第四纪海侵的新构造背景[J].地质力学学报,1999,4(4):42-48.
[WANG Qiang, TIAN Guoqiang. The neotectonic setting of Late Quaternary transgressions on the eastern coastal plain of China[J]. Journal of Geomechanics, 1999, 4(4):41-48
[12] WANG Qiang, YUAN Guibang, HU Yunzhuang, et al. Microfossils in tidal flat strata on the northern Huanghua area since the MIS3[J]. Acta Micropalaeontologica Sinica, 2008, 25(1):1-18.
[13] 王强,吕金福.海面变化与海岸变迁[M]//见:李汉鼎,吕金福,王强,等.中国北方沿海泥炭与环境.北京:海洋出版社,1995:109-128.[WANG Qiang, LÜ Jinfu. Eustacy and coastline movement[C]//In:LI Handing, LÜ
; Jinfu, WANG Qiang, et al. Peat and Environment on Coastal Area of the North China. Beijing:China Ocean Press, 1995:109-128.]
[14] 李广雪,杨子赓,刘勇.中国东部海域海底沉积环境成因研究[M].北京:科学出版社,2005:1-44.[LI Guangxue, YANG Zigeng, LIU Yong. Formation Environment of the Seafloor Sediment in the Eastern China Seas[M]. Beijing:Science Press, 2005:1
-44.]
[15] Klein G D. A sedimentary model for determining paleotidal range[J]. Bulletin of Geological Society of America, 1971,82:2582-2592.
[16] 施雅风,于革.40~30kaBP.中国暖湿气候和海侵的特征与成因探讨[J].第四纪研究,23(1):1-11[SHI Yafeng, YU Ge. Warm-humid climate and transgressions during 40
-30 kaBP and their potential mechanisms[J]. Quaternary Sciences, 2003, 23(1):1-11.]
[17] 王强,袁桂邦,张熟,等.渤海湾西岸贝壳堤堆积与海陆相互作用[J].第四纪研究,2007,27(5):775-786.
[WANG Qiang, YUAN Guibang, ZHANG Shu, et al. Shelly ridge accumulation and sea-land interaction on the west coast of the Bohai Bay[J]. Qua. Sci., 2007,27(5):775-786.]
[18] 汪品先.海洋微体古生物论文集[M].北京:海洋出版社,1980:1-204.[WANG Pinxian, Papers on Marine Micropalaeontology[M]. Beijing:China Ocean Press, 1980:1
-204.]
[19] 何起祥,张明书.中国西沙礁相地质[M].北京:科学出版社,1986:147-168.[HE Qixiang, ZHANG Mingshu. Reef Geology of the Xisha Islands[M]. Beijing:Science Press, 1986:147
-168.]
[20] 王强,张玉发,袁桂邦,等.MIS3阶段以来黄骅北部地区海侵与气候期对比[J].第四纪研究,2008,28(1):79-95.
[WANG Qiang, ZHANG Yufa, YUAN Guibang, et al. Since MIS3 stage the correlation between transgression and climatic change in the north Huanghua area, Hebei[J]. Qua. Sci., 2008, 28(1):79-95.]
[21] 郑守仪,郑执中,王喜堂,等.山东省打渔张灌区第四纪有孔虫及其沉积环境的初步研究[J].海洋科学集刊,1978,13:16-88.[ZHENG Shouyi, CHENG Tsichung, WANG Xitang, et al. The foraminifera of the Dayuzhang irrigation area, Shandong Province, and a preliminary attempt at an interpretation of its depositional environment[J].Studia Marine Sinica, 1978
, 13:16-88.]
[22] 赵长荣, Hus J, 阎玉忠,等.渤海湾西岸湾顶晚更新世-全新世年代地层序列与地磁极漂移[J].地质调查与研究,2003,26(3):183-192.
[ZHAO Changrong,Hus J,YAN Yuzhong, et al. Late Pleistocene-Holocene chronostratigraphic sequence and the geomagnetic polar excursion on the west coast of Bohai Bay[J]. Geological Servey and Reserch., 2003,26(3):183-192.]
[23] 陈宇坤,李振海,邵永新,等.天津地区第四纪年代地层剖面研究[J].地震地质,2008,30(2):383-399.
[CHEN Yukun,LI Zhenhai,SHAO Yongxin, et al. Study on the Quaternary chronostratigraphic section in Tianjin area[J]. Seismology and Geology, 2008,30(2):383-399.]
[24] 李从先,陈刚,姚明.我国河流输砂对海岸和大陆架的影响[J].同济大学学报,1988,16(2):137-146.
[LI Congxian, CHEN Gang, YAO Ming. The influence of river discharge for coast and shelf in China[J]. Journal of Tongji University, 1988, 16(2):137-146.]
[25] 武汉地质学院北京研究生院石油地质岩相组,大港油田石油勘探开发研究院勘探室岩相组.黄骅坳陷第三系沉积相及沉积环境[M].北京:地质出版社,1987:1-180.[Petro-Lithological Group of Wuhan Geological College and Lithological Group of Petro-Exploration and Develop Institute, Dagang Oil Field. Tertiary System Sedimentary Facies and Environment of Huanghua Depression[M]. Beijing:Geol. Publ. House, 1987:1
-180.]
[26] Mial A D. The Geology of Fluvial Deposits[M]. Springer, 1996:343-378.
[27] Emery D, Myers K. Sequence Stratigraphy[M]. Blackwell Science, 1996:111-133.
[28] Catuneanu O.Principles of Sequence Stratigraphy[M]. Elsevier, 2006:246-253.
[29] 刘招君,董清水,王嗣敏,等. 陆相层序地层学导论与应用[M]. 北京:石油工业出版社,2002:1-55.[LIU Zhaojun, DONG Qingshui, WANG Simin, et al. Introduction to Continental Sequence Stratigrahy & Application[M]. Beijing:Petroleum Industry Press, 2002:1
-55.]
[30] 马正.应用自然电位测井曲线解释沉积环境[J].石油与天然气地质,1982,3(1):25-40.
[MA Zheng. Utilization of the combination of log shapes for explanation of the sedimentary environment[J]. Oil & Gas Geology, 1982,3(1):25-40.]
[31] 李从先.滦河冲积扇-三角洲沉积体系[M].北京:地质出版社,1985:1-158.[LI Congxian. The Luanhe Fan-delta Deposits System[M]. Beijing:Geol. Publ. House,1985:1
-158.]
[32] 郭彦如,刘全新,樊太亮,等.查干断陷湖盆层序地层框架中的含油气系统[M].北京:地质出版社,2003:1-136.[GUO Yanru, LIU Quanxin, FAN Tailiang, et al. Oil and Gas System in the Sequence Stratigraphy Fragment of Chagan Fault-Depressed Lake Basin[M]. Beijing:Geol. Publ. House,2003:1
-136.]
[33] 赵国敏,赵根模,陈宇坤,等. 天津海河断裂活动性研究[M]. 北京:地震出版社,2006:36-124.[ZHAO Guomin, ZHAO Genmo, CHEN Yukun, et al. Study on the Activity of Haihe Fault in Tianjin[M]. Beijing:Seismic Press, 2006:36
-124.]
[34] 安芷生,王苏民,吴锡浩,等.中国黄土高原的风积证据:晚新生代北半球大冰期开始及青藏高原的隆升驱动[J]. 中国科学D辑,1998,28(6):481-490.
[AN Zhisheng, WANG Sumin, WU Xihao, et al. The aeolian evidence of loess accumulation in China Loess Plateau:The start of great glacial stage of North Hemisphere since Late Cenozoic and driving of Tibet Plateau uplifting[J]. Science in China (Ser. D), 1998, 28(6):481-490.]
[35] 张克信,王国灿,曹凯,等. 青藏高原新生代主要隆升事件:沉积响应与热年代学记录[J]. 中国科学D辑,2008,38(12):1575-1588.
[ZHANG Kexin, WANG Guocan, CAO Kai, et al. Since Cenozoic the major uplifting events of Tibet Plateau:Sediments response and thermal-chronological records[J]. Science in China (Ser. D), 2008, 38(12):1575-1588.]
[36] 李从先,范代读,杨守业,等.中国河口三角洲地区晚第四纪下切河谷层序特征和形成[J].古地理学报,2008,10(1):87-97.
[LI Congxian, FAN Daidu, YANG Shouye, et al. Characteristics and formation of Late Quaternary incised-valley sequence in estuary and delta areas in China[J]. Journal of Palaeogeography, 2008,10(1):87-97.]
[37] 吴标云,李从先.长江三角洲地区第四纪地质[M].北京:地质出版社,1988:1-151.[WU Biaoyun, LI Congxian. Quaternary Geology of Changjiang Delta[M]. Beijing:Geol. Publ. House, 1988:1
-151.]
-
计量
- 文章访问数: 1067
- PDF下载数: 7
- 施引文献: 0
下载: