北京平原区南部PGZ01孔第四纪地层划分及其环境意义<sup>*</sup>

doi:10.7605/gdlxb.2018.02.025

古地理学报 ›› 2018, Vol. 20 ›› Issue (2): 337-348. doi: 10.7605/gdlxb.2018.02.025

• 第四纪古地理学及沉积学 • 上一篇

北京平原区南部PGZ01孔第四纪地层划分及其环境意义^*

赵勇¹, 王强², 李瑞杰¹, 魏波¹, 徐吉祥³, 孙永华¹, 张晓亮¹, 王纯君¹, 周圆心¹, 尤世娜¹, 吕金波¹

1 北京市地质调查研究院,北京 100195;
2 中国地质调查局天津地质调查中心,天津 300170;
3 北京市地质矿产勘查开发局,北京 100195

收稿日期:2016-04-05 修回日期:2017-11-23 出版日期:2018-04-01 发布日期:2018-04-02
通讯作者: 王强,男,1945年生,天津地质调查中心研究员,研究方向为第四纪地质与海洋地质。E-mail: tjwq1945@163.com。
作者简介:赵勇,男,1983年生,毕业于中国地质大学(北京)构造地质学专业,现为北京市地质调查研究院高级工程师,研究方向为区域地质与第四纪地质。E-mail: zhaoyong3068@163.com。
基金资助:
*中国地质调查局北京1:5万琉璃河、庞各庄、安次县幅区调项目(编号: 12120114007701)和国家自然科学基金项目(编号: 40872107)共同资助

Quaternary stratigraphic division and its environmental significance of Borehole PGZ01 in southern Beijing plain area

Zhao Yong¹, Wang Qiang², Li Rui-Jie¹, Wei Bo¹, Xu Ji-Xiang³, Sun Yong-Hua¹, Zhang Xiao-Liang¹, Wang Chun-Jun¹, Zhou Yuan-Xin¹, You Shi-Na¹, Lü Jin-Bo¹

1 Beijing Geological Survey Institute,Beijing 100195;
2 Tianjin Geological Survey Centre,China Geological Survey Bureau,Tianjin 300170;
3 Beijing Geology and Mineral Resources Exploration and Development Bureau,Beijing 100195

Received:2016-04-05 Revised:2017-11-23 Online:2018-04-01 Published:2018-04-02
Contact: Wang Qiang,born in 1945,is a professor at Tianjin Geological Survey Centre. He is mainly engaged in Quaternary geology and marine geology. E-mail: tjwq1945@163.com.
About author:Zhao Yong,born in 1983,is a senior engineer at Beijing Institute of Geological Survey. He is mainly engaged in regional and Quaternary geology. E-mail: zhaoyong3068@163.com.About the corresponding author Wang Qiang,born in 1945,is a professor at Tianjin Geological Survey Centre. He is mainly engaged in Quaternary geology and marine geology. E-mail: tjwq1945@163.com.
Supported by:
[Co-funded by Beijing 1:50 000 Liulihe,Panggezhuang,Ancixian Regional Geological Survey Project of China Geological Survey(No. 12120114007701) and the National Natural Science Foundation of China(No. 40872107)]

摘要/Abstract

摘要：

对北京平原区南部大兴榆垡镇420m 深的PGZ01孔岩心进行了岩石地层、磁性地层、¹⁴C测年、介形类组合和孢粉组合研究。结果表明:(1)Matuyama(松山)/Gauss(高斯)和Brunhes(布容)/Matuyama(松山)极性界线分别位于280m和78.35m处,钻孔底部已经进入Gauss正极性带;取280m处Matuyama/Gauss极性界线作为第四系下限,显示可能的永定河泥石流—冲积扇在第四纪之前即到达了北京平原南部,但是华北平原上新统标志岩石地层单元——厚层棕红色黏土在Olduvai(奥尔都维)极性亚带之上即已出现。(2)结合AMS¹⁴C测年,尝试将约60m以上地层的氧化—还原状况,与对古季风影响反映灵敏的沿海平原钻孔同样深度地层进行对比,继而确定上更新统和全新统的底界深度分别位于56.60m和18.95m。(3)MIS5(海洋同位素阶段)以来的特征沉积物,与沿海平原钻孔地层有很好的可比性,同时也有8~4ka期间史前大洪水的影响。本研究为廊(坊)固(安)凹陷西北边缘区第四纪地层划分对比、古地理环境演化、活动断裂以及区域差异构造沉降研究,提供了重要的年代地层格架,对理解晚更新世以来古季风变化的环境效应有重要的启迪。

关键词: 磁性地层, 第四系, 古永定河, 廊固凹陷, 北京平原区

Abstract:

Based on the core materials collected from the Borehole PGZ01,which is located at Yufa Township of Daxing district in southern Beijing plain area and has a depth of 420m,the analyses of lithostrotigraphy,magnetostratigraphy,AMS ¹⁴C dating,Ostracoda and sporopollen assemblages were carried out. The results show that: (1)The boundaries of Matuyama/Gauss polarity chron and Brunhes/Matuyama polarity chron appear at the depth of 280m and 78.35m, respectively. It suggests that the bottom strata of this borehole correspond to Gauss normal polarity zone at the bottom. Considering that the boundary of Matuyama/Gauss polarity chron at the depth of 280m is the lower boundary of Quaternary system. It suggests that the debris flow and alluvial fan or possible palaeo-Yongding River had arrived at the southern part of Beijing plain area before Quaternary. Moreover, thick-layer brownish red clay which is considered as the upper mark lithostratigraphic unit of the Pliocene occurred at the Olduvai subzone. (2)Integrated with the AMS ¹⁴C dating,the present study tentatively correlate the stratal oxidation-reduction status above the depth of 60m to correlate to cores from palaeomonsoonal-sensitive coastal plain environment,the boundary of the Upper Pleistocene and Holocene was determined to be at 56.60m and 18.95m, respectively. (3)The characteristic sediments deposited since MIS5 have a good correlation with core sediments from coastal plain environment,and show evidence of the influence of Prehistoric Flood of 8-4ka. The present paper provided important age control for subdividion and correlation of Quaternary stratigraphy,construction of palaeogeography,fault activities and tectonic history of the westnorthern margin region of Lang(fang)-Gu(an) Depression,and understanding of the environmental effect of palaeomonsoon change since the Late Pleistocene.

Key words: magnetostratigraphy, Quaternary, palaeo-Yongding River, Beijing plain area

中图分类号:

P534.63

赵勇, 王强, 李瑞杰, 魏波, 徐吉祥, 孙永华, 张晓亮, 王纯君, 周圆心, 尤世娜, 吕金波. 北京平原区南部PGZ01孔第四纪地层划分及其环境意义^*[J]. 古地理学报, 2018, 20(2): 337-348.

Zhao Yong, Wang Qiang, Li Rui-Jie, Wei Bo, Xu Ji-Xiang, Sun Yong-Hua, Zhang Xiao-Liang, Wang Chun-Jun, Zhou Yuan-Xin, You Shi-Na, Lv Jin-Bo. Quaternary stratigraphic division and its environmental significance of Borehole PGZ01 in southern Beijing plain area[J]. JOPC, 2018, 20(2): 337-348.

http://www.gdlxb.cn/CN/Y2018/V20/I2/337

参考文献

[1] 安芷生,魏兰英,卢演俦,王乃文,何希贤,丁申. 1979. 顺5孔的磁性地层学和早期松山世的北京海侵. 地球化学, 8(4): 343-345. [An Z S,Wei L Y,Lu Y C,Wang N W,He X X,Ding S. 1979. Magnetostraigaphy of the core S-5 and the transgression in Beijing area during the early Matuyama Epoch. Geochimica, 8(4): 343-345]
[2] 蔡向民,郭高轩,栾英波,梁亚楠. 2009a. 北京山前平原区第四系三维结构调查方法研究. 地质学报, 83(7): 1047-1056. [Cai X M,Guo G X,Luan Y B,Liang Y N. 2009a. Quaternary geological features of Beijing piedmont plain using 3D structural method. Acta Geologica Sinica, 83(7): 1047-1056]
[3] 蔡向民,栾英波,郭高轩,梁亚楠. 2009b. 北京平原第四系的三维结构. 中国地质, 36(5): 1021-1029. [Cai X M,Luan Y B,Guo G X,Liang Y N. 2009b. 3D Quaternary geological structure of Beijing plain. Geology in China, 36(5): 1021-1029]
[4] 蔡向民,郭高轩,栾英波,孙知明,梁亚南,姜龙群. 2010. 永定河形成时代研究. 第四纪研究, 30(1): 167-174. [Cai X M,Guo G X,Luan Y B,Sun Z M,Liang Y N,Jiang L Q. 2010. Forming time for the Yongding River. Quaternary Sciences, 30(1): 167-173]
[5] 高秀林,王强,李玉德,杜乃秋,孔昭宸. 1986. 从天津P8孔看中更新世末期以来海侵期、气候期对比问题. 海洋地质与第四纪地质, 6(1): 53-65. [Gao X L,Wang Q,Li Y D,Du N Q,Kong Z C. 1986. On correlations between transgressions and climatic phases since late Middle-Pleistocene based on data of drilling hole P8 in Tianjin. Acta Ocenological Sinica,6(supp.Ⅱ): 153-166]
[6] 胡云壮,张金起,白耀楠,夏雨波,王强. 2014a. 3.45Ma以来滦河冲积扇中部唐山TD1孔记录的区域构造和气候演化. 古地理学报, 16(2): 249-262. [Hu Y Z,Zhang J Q,Bai Y N,Xia Y B,Wang Q. 2014a. Records of regional tectonic and climatic evolution since 3.45Ma at borehole TD1 of Tangshan in the middle part of Luanhe river fluvial fan. Journal of Palaeogeography(Chinese Edition), 16(2): 249-262]
[7] 胡云壮,胥勤勉,袁桂邦,裴军令,杨吉龙,张玉发,王强. 2014b. 河北海兴小山CK3孔磁性地层与第四纪火山活动记录. 古地理学报, 16(3): 411-426. [Hu Y Z, Xu Q M, Yuan G B, Pei J L, Yang J L, Zhang Y F, Wang Q. 2014b. Magnetostratigraphy in the borehole CK3 and record of Quaternary volcanic activity in Xiaoshan area of Haixing,Hebei Province. Journal of Palaeogeography(Chinese Edition), 16(3): 411-426]
[8] 李龙吟,陈华慧. 1994. 北京怀柔HR88-1钻孔剖面磁性地层学研究. 地层学杂志, 18(1): 39-44. [Li L Y,Chen H H. 1994. On magnetostratigraphy of the borehole HR88-1 in Huairou area Beijing. Journal of Stratigraphy, 18(1): 39-44]
[9] 李天杰,郑应顺,王云. 1983. 土壤地理学(第二版).北京: 高等教育出版社,113-135. [Li T J,Zheng Y S,Wang Y. 1983. Soil Geography(Second Edition). Beijing: Higher Education Press,113-135]
[10] 李小艳,赵泉鸿,姚政权,王强,翦知湣,石学法. 2015. 渤海百万年以来的海侵记录: BH08孔有孔虫和介形类证据. 海洋地质与第四纪地质, 35(6): 93-108. [Li X Y,Zhao H Q,Yao Z Q,Wang Q,Jian Z M,Shi X F. 2015. Transgressive records of last million years in the Bohai Sea. Marine Geology & Quaternary Geology, 35(6): 93-108]
[11] 刘东生,施雅风,王汝建,赵泉鸿,翦知湣,成鑫荣,汪品先,王苏民,袁宝印,吴新智,邱占祥,徐钦琦,黄万波,黄慰文,安芷生,鹿化煜. 2000. 以气候变化为标志的中国第四纪地层对比表. 第四纪研究, 20(2): 108-128. [Liu T S,Shi Y F,Wang R J,Zhao Q H,Jian Z M,Cheng X R,Wang P X,Wang S M,Yuan B Y,Wu X Z,Qiu Z X,Xu Q Q,Huang W B,Huang W W,An Z S,Lu H Y. 2000. Table of Chinese Quaternary stratigraphic correlation remarked with climate change. Quaternary Sciences, 20(2): 08-128]
[12] 栾英波,郭高轩,黄骁. 2008a. 北京山前冲洪积缓倾斜平原晚新生代沉积物磁性地层学研究. 城市地质, 3(2): 17-20. [Luan Y B,Guo G X,Huang X. 2008a. A magnetostraigraphic study of Upper Cenozoic sediments in Beijing's gently-sloping alluvial piedmont plain. City Geology, 3(2): 17-20]
[13] 栾英波,郭莉,郭高轩,黄骁. 2008b. 北京地区新5孔第四纪松散沉积物的微量元素地球化学特征及古气候、古环境研究. 城市地质, 3(3): 18-22. [Luan Y B,Guo L,Guo G X,Huang X. 2008b. Geochemical Characters of trace elements from well Xin-5 in Quaternary sediments and studies of paleoclimate and paleoenvironment. City Geology, 3(3): 18-22]
[14] 栾英波,蔡向民,郭高轩,梁亚楠,郭莉. 2011. 北京平原区新5孔岩心特征及地层初步划分. 中国地质, 38(2): 495-503. [Luan Y B,Cai X M,Guo G X,Liang Y N,Guo L. 2011. Core characteristics and preliminary stratigraphic classification of the New-5 hole in Beijing Plain. Geology in China, 38(2): 495-503]
[15] 王丽艳,李广雪. 2016. 古气候替代性指标的研究现状及应用. 海洋地质与第四纪地质, 36(4): 153-161. [Wang L Y,Li G X. 2016. Research status and application of paleoclimatic proxies. Marine Geology & Quaternary Geology, 36(4): 153-161]
[16] 王强. 1999. 渤海西岸全新世早期基底泥炭堆积时间域初步研究. 第四纪研究, 19(1): 91-96. [Wang Q. 1999. Preliminary study on the time domain of basal peat accumulation in the early Holocene in the west Bohai Bay. Quaternary Sciences, 19(1): 91-96]
[17] 王强,吕金福. 1995. 第十章: 海面变化与海岸线变迁. 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,109-128. [Wang Q,Lü J F. 1995. Chapter 10,Eustacy and coastal movement. In: Li H D,Lü J F,Wang Q et al . 1995. Peat and Environment on Coastal Area of the North China. Beijing: China Ocean Press,109-128]
[18] 王强,田国强. 1999. 中国东部晚第四纪海侵的新构造背景. 地质力学学报, 4(1): 42-48. [Wang Q,Tian G Q. 1999. The neotectonic setting of Late Quaternary transgressions on the eastern coastal plain of China. Journal of Geomechanics, 4(1): 42-48]
[19] 王强,李从先. 2009. 中国东部沿海平原第四系层序类型. 海洋地质与第四纪地质,26 (4):39-51.[Wang Q, Li C X. 2009. The type of Quaternary sequence in the east China coastal plain. Marine Geology & Quaternary Geology, 26(4): 39-51]
[20] 王强,李凤林,李玉德,高秀林. 1986. 对渤海西、南岸平原第四纪海侵命名的讨论. 海洋学报, 8(1): 72-82. [Wang Q,Li F L,Li Y D, Gao X L. 1987. Discussion on the naming of the Quaternary transgressions in west-southrn coastal plain of the Bohai Sea. Acta Oceanologica Sinica, 6(1): 104-115]
[21] 王强,宋大伟,王云生. 1992. 第七章第四系. 见:邓永高(主编).中华人民共和国地质矿产部地质专报,一,区域地质,第29号: 天津市区域地质志. 北京:地质出版社,116-156. [Wang Q, Song D W, Wang Y S. 1992. 7th Chapter, Quaternary System. Deng Y G (ed). PR China, Ministry of Geol. & Min. Res., Geol. Memoirs, ser.1, No.29, Regional Geology of Tianjin Municipality. Beijing: Geological Publishing House, 116-156]
[22] 王强,刘立军,徐海振,马震,职太平,兰自亭,王亚斌,刘雪松,林沛,董殿伟. 2003. 华北平第四系下限的再研究. 地质调查与研究, 26(1): 52-60. [Wang Q,Liu L J,Xu H Z,Ma Z,Zhi T P,Lan Z T,Wang Y B,Liu X S,Lin P,Dong D W. 2003. Re-study on the lower boundary of Quaternary system in the North China Plain. Geological Survey and Research, 26(1): 52-60]
[23] 王强,张玉发,袁桂邦,张文卿. 2008. MIS3阶段以来河北黄骅北部地区海侵期与气候期的对比. 第四纪研究, 28(1): 79-95. [Wang Q,Zhang Y F,Yuan G B,Zhang W Q. 2008. Since MIS3 the correlation between transgression and climatic changes in the north Huanghua area,Hebei. Quaternary Sciences, 28(1): 79-95]
[24] 吴胜和,冯文杰,印森林,喻宸,张可. 2016. 冲积扇沉积构型研究进展. 古地理学报, 18(4): 497-512. [Wu S H,Feng W J,Yin S L,Yu C,Zhang K. 2016. Research advances in alluvial fan depositional architecture. Journal of Palaeogeography(Chinese Edition), 18(4): 497-512]
[25] 肖国强,杨吉龙,赵长荣,王强,胥勤勉,胡云壮,秦雅飞,李静,肖国桥. 2014. 天津滨海地区G2孔磁性地层年代及其构造指示. 地质通报, 33(10): 1642-1650. [Xiao G Q,Yang J L,Zhao C R,Wang Q,Hu Y Z,Qin Y F,Li J,Xiao G Q. 2014. Magnetostratigraphy of drill hole G2 in the Tianjin coastal area and its tectonic significance. Geological Bulletin of China, 33(10): 1642-1650]
[26] 袁宝印,邓成龙,吕金波,金昌柱,吴玉书. 2002. 北京平原晚第四纪堆积期与史前大洪水. 第四纪研究, 22(5): 474-480. [Yuan B Y,Deng C L,Lü J B,Jin C Z,Wu Y S. 2002. A Late Quaternary accumulation period and the prehistoric flood in Beijing plain. Quaternary Sciences, 22(5): 474-480]
[27] 杨子赓,谢又予,牟均智. 1983. 周口店上新世及更新世的古气候与地层. 地质论评, 29(3): 209-219. [Yang Z G,Xie Y Y,Mou J Z. 1983. Study of palaeo-climatology and stratigraphy of the Pliocene and Pleistocene at Zhoukoudian. Geological Review, 29(3): 209-219]
[28] 张青松,李元芳,邢嘉明,濮静娟. 1976. 水系变迁与新构造运动. 地理集刊,第10号:71-82. [Zhang Q S,Li Y F,Xing J M,Pu J J. 1976. Changes of river system and new tectonic movement. Geographical Society,10:71-82]
[29] 赵松龄,杨光复,苍树溪,张宏才,黄庆福,夏东兴,王永吉,刘福寿,刘成福. 1978. 关于渤海湾西岸海相地层与海岸线问题. 海洋与湖沼,(9): 15-25. [Zhao S L,Yang G F,Cang S X,Zhang H C,Huang Q F,Xia D X,Wang Y J,Liu F S,Liu C F. 1978. On the marine stratigraphy and coastlines of the western coast of the gulf of Bohai. Oceannologia and Liminologia, 9(1): 15-25]
[30] 赵勇,蔡向民,王继明,吴怀春,白凌燕,张磊,何静,何付兵. 2013. 北京平原顺义ZK12-2钻孔剖面第四纪磁性地层学研究. 地质学报, 87(2): 288-294. [Zhao Y,Cai X M,Wang J M,Wu H C,Bai L Y,Zhang L,He J,He F B. 2013. Magnetostratigraphy of ZK12-2 borehole in Shunyi area,Beijing Plain. Acta Geologica Sinica, 87(2): 288-294]
[31] 赵勇,蔡向民,王继明,张磊,刘予,吕金波. 2015. 北京平原构造断块划分及微断块第四纪活动性探讨. 中国地质,42(6): 1876-1884. [Zhao Y,Cai X M,Wang J M,Zhang L,Liu Y,Lü J B. 2015. The division of “small blocks”of structure in Beijing plain and a discussion on the activity of micro-block in Quaternary period. Geology in China,42(6): 1876-1884]
[32] 周昆叔,严富华,梁秀龙. 1978. 北京平原第四纪晚期花粉分析及其意义. 地质科学,(1): 57-64. [Zhou K S,Yan F H,Liang X L. 1978. Pollen analysis of Late Quaternary in Beijing plain and its significance. Chinese Journal of Geology,(1): 57-64]
[33] Parham P R, Riggs S R, Culver S J, Mallinson D J,W. Jackrink W, Kevin B K. 2013. Quaternary coastal lithofacies,sequence development and stratigraphy in a passive margin setting,North Carolina and Virginia,USA. Sedimentology,60:503-547.
[34] Singer B S. 2014. A Quaternary geomagnetic instability time scale. Quaternary Geochronology, 24(1): 29-52.
[35] Tänavsuu-Milkeviciene K. Frederick S J. 2012. Evolution of an organic-rich lake basin-stratigraphy,climate and tectonics: Piceance Creek basin,Eocene Green River Formation. Sedimentology, 59(6): 1735-1768.
[36] Toker E,Kayserl-Ozer M S,Ozkul M,Kele S. 2015. Depositional system and palaeoclimatic interpretations of Middle to Late Pleistocene travertines: Kocabas,Denizli,south-west Turkey. Sedimentology, 62(5): 1360-1383.
[37] Wunsch M,Betzler C,Lindhorst S,Lüdmann T,Eberli G P. 2017. Sedimentary dynamics along carbonate slopes(Bahamas archipelago). Sedimentology, 64(4): 631-657.
[38] Yao Z Q,Shi X F,Liu Q S,Liu Y G,Juan Cruz Larrasoaña,Liu J X,Ge S L,Wang K S,Qiao S Q,Li X Y,Shi F D,Fang X S,Yu Y G,Yang G,Duan Z Q. 2014. Paleomagnetic and astronomical dating of sediment core BH08 from the Bohai Sea,China: Implications for glacial-interglacial sedimentation. Palaeogeography, Palaeoclimatology, Palaeoecology, 393: 90-101.

选择文件类型/文献管理软件名称

选择包含的内容

北京平原区南部PGZ01孔第四纪地层划分及其环境意义^*

Quaternary stratigraphic division and its environmental significance of Borehole PGZ01 in southern Beijing plain area

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 11

编辑推荐

Metrics

本文评价

[1]	施源, 刘卫红, 邱隆伟, 高雪峰, 董道涛, 王宇喆. 柴达木盆地七个泉背斜狮子沟组与七个泉组构造-沉积演化及对砂岩型铀矿成矿的启示^*[J]. 古地理学报, 2024, 26(3): 700-713.
[2]	易定红, 刘应如, 李积永, 刘俊丰, 奎明清, 陈汾君, 吴颜雄, 张婷静, 李红哲, 倪帅. 柴达木盆地三湖地区第四系七个泉组物源研究^*[J]. 古地理学报, 2024, 26(3): 644-654.
[3]	李瑞杰, 王强, 赵勇, 魏波, 孙永华. 河北平原廊固凹陷ACX03孔晚上新世以来地层与沉积^*[J]. 古地理学报, 2021, 23(3): 539-554.
[4]	孙振营, 王强, 李亚平, 裴军令, 周相国, 高学飞. 第四纪以来天津北部燕山隆升与山前盆地的形成^*[J]. 古地理学报, 2018, 20(5): 893-908.
[5]	鲁庆伟, 王强, 詹健, 郭维, 李稳, 王西玉. 渤海湾西岸沧县隆起中更新世地层间断^*[J]. 古地理学报, 2018, 20(4): 665-679.
[6]	胡云壮, 胥勤勉, 袁桂邦, 裴军令, 杨吉龙, 张玉发, 王强. 河北海兴小山CK3孔磁性地层与第四纪火山活动记录*[J]. 古地理学报, 2014, 16(3): 411-426.
[7]	陈慧娴, 骆美美, 王建华, 苏志华, 金刚雄, 瓦西拉里, 杨小强, 曹玲珑. 福建九龙江河口第四纪沉积物特征及沉积环境演变[J]. 古地理学报, 2014, 16(2): 263-273.
[8]	胡云壮, 张金起, 白耀楠, 夏雨波, 王强. 3.45 Ma以来滦河冲积扇中部唐山TD1孔记录的区域构造和气候演化[J]. 古地理学报, 2014, 16(2): 249-262.
[9]	李华, 王英民, 徐强, 唐武, 李冬. 南海北部第四系深层等深流沉积特征及类型*[J]. 古地理学报, 2013, 15(5): 741-750.
[10]	操应长, 葸克来, 王艳忠, 周磊, 赵贤正, 金凤鸣, 崔周旗, 杨春宇, 董雄英. 冀中坳陷廊固凹陷河西务构造带古近系沙河街组四段储集层孔隙度演化定量研究[J]. 古地理学报, 2013, 15(5): 593-604.
[11]	李鑫, 钟大康, 李勇, 雷刚林, 杨宪彰, 吴庆宽, 胡顺庆, 祝海华. 塔里木盆地库车坳陷新近系和第四系沉积特征及演化^*[J]. 古地理学报, 2013, 15(2): 169-180.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

北京平原区南部PGZ01孔第四纪地层划分及其环境意义*

Quaternary stratigraphic division and its environmental significance of Borehole PGZ01 in southern Beijing plain area

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 11

编辑推荐

Metrics

本文评价

北京平原区南部PGZ01孔第四纪地层划分及其环境意义^*