Sedimentary Characteristics and Evolution of the Upper Sinian#br#
Doushantuo Formation in the North of Middle Yangtze Area

doi:10.11885/j.issn.1674-5086.2014.09.17.02

Abstract

Abstract:

A large set of dark grey to black colored mudstone and shale deposited in the middle to lower part of the upper
Sinian Doushantuo Formation in the middle Yangtze Platform，most of which are deeply buried in the Basin and with a good
shale gas resource potential. Based on drilling cores and outcrop section investigation，a systematical study on fundamental
geology was carried out. We also analyzed the sequence stratigraphy and sedimentary facies of the Doushantuo Formation，and
established regional stratigraphic framework. The lithology of the upper Sinian Doushantuo Formation is characteristic of four
different lithofacies，and the thickness of which is different in drilling cores and outcrop sections with variation ranges from 90
to 250 m. In general，the stratum is thickening along the direction of northwest to southeast. Doushantuo Formation was divided
into a second-order sequence（SS1），which contains four third-order sequences（SQ1、SQ2、SQ3、SQ4）. Sedimentary facies of
Doushantuo Formation were subdivided into tidal-flat and platform with three subfacies as open platform，shallow water shelf
and intra-platform basin respectively. In Doushantuo period，the sedimentary environments of Doushantuo Formation varied
from southeast to northwest as open platform and restricted platform in the study area，intra-platform basin face in the area of
Huajipo，Well X1 and Jiuliya.

Key words: stratigraphic characteristics, sedimentary facies, Upper Sinian, Doushantuo Formation, the north of middle
Yangtze area

CLC Number:

TE121

SHAN Changan1, ZHANG Tingshan1*, ZHANG Zhao2, GUO Junjie1，3. Sedimentary Characteristics and Evolution of the Upper Sinian#br# Doushantuo Formation in the North of Middle Yangtze Area[J]. 西南石油大学学报(自然科学版), DOI: 10.11885/j.issn.1674-5086.2014.09.17.02.

0
/ / Recommend

Add to citation manager EndNote|Ris|BibTeX

URL: http://journal15.magtechjournal.com/Jwk_xnzk/EN/10.11885/j.issn.1674-5086.2014.09.17.02

http://journal15.magtechjournal.com/Jwk_xnzk/EN/Y2016/V38/I3/1

References

[1] 王韶华. 中扬子震旦统油气藏特征及勘探潜力[D]. 武
汉：中国地质大学，2010.
WANG Shaohua. Hydrocarbon accumlation characteristics
and exploration potential of the upper Sinian in the
middle Yangtze Area[D]. Wuhan：China University of
Geosciences，2010.
[2] 万天丰. 中国大陆早古生代构造演化[J]. 地学前缘，
2006，13（6）：30 42.
WAN Tianfeng. Tectonic evolution in the Chinese continent
from middle Cambrian to early Devonian[J]. Earth
Science Frontiers，2006，13（6）：30 42.
[3] 王鸿祯. 中国地壳构造发展的主要阶段[J]. 地球科学，
1982，18（3）：28 36.
WANG Hongzhen. The main stages of Crustal development
of China[J]. Earth Science，1982，18（3）：28 36.
[4] 湖北省地矿局. 区域地质调查报告1：20 万（南漳幅
H 49 IV）[R]. 1982：41 43.
[5] 湖北省区域地质测量队. 区域地质报告1：20 万（宜昌
幅H 49 X 和长阳幅H 49 XVI）[R]. 1970：16 21.
[6] 湖北省地矿局. 区域地质调查报告1：20 万（宜城幅
H 49 V 和随县幅H 49 VI）[R]. 1982：43 88.
[7] 湖北省地矿局. 区域地质调查报告1：20 万（钟祥幅
H 49 XI 和应城幅H 49 XII）[R]. 1982：23 48.
[8] 马国干，李华芹，张自超. 华南地区震旦纪时限范围的
研究[J]. 中国地质科学院宜昌地质矿产研究所所刊，
1984（8）：1 29.
MA Guogan，LI Huaqin，ZHANG Zichao. An investigation
of the age limits of the Sinian system in South
China[J]. Bulletin of the Yichang Institute of Geology and
Mineral Resources，Chinese Academy of Geological Sciences，
1984（8）：1 29.
[9] 马国干，张自超，李华芹，等. 扬子地台震旦系同位素
年代地层学的研究[J]. 中国地质科学院宜昌地质矿产
研究所所刊，1989（14）：114 123.
MA Guogan，ZHANG Zichao，LI Huaqin，et al. The study
of isotope chronostratigraphy about the Sinian，Yangtze
Region[J]. Bulletin of the Yichang Institute of Geology
and Mineral Resources，Chinese Academy of Geological
Sciences，1989（14）：114 123.
[10] 丁启秀，陈忆元. 湖北峡东地区震旦纪软躯体后生动
物的发现及意义[J]. 地球科学，1981（2）：53 57.
DING Qixiu，CHEN Yiyuan. The discovery and significance
of software metazoan from Sinian in the Xiadong region，
Hubei Province[J]. Earth Science，1981（2）：53 57.
[11] 解古巍，周传明，McFadden K A，等. 湖北峡东地区九
龙湾剖面震旦系陡山沱组微体化石的新发现[J]. 古生
物学报，2008，47（3）：279 291.
XIE Guwei，ZHOU Chuanming，MCFADDEN K A，et
al. Microfossils discovered from the Sinian Doushantuo
Formation in the Jiulongwan section，east Yangtze Gorges
Area，Hubei Province，south China[J]. Acta Palaeontologica
Sinica，2008，47（3）：279 291.
[12] 陈孟莪，肖宗正，袁训来. 晚震旦世的特种生物群
落庙河生物群新知[J]. 古生物学报，1994，33（4）：
391 403.
CHEN Meng′e，XIAO Zongzheng，YUAN Xunlai. A new
assemblage of megafossils Miaohe biota from upper
Sinian Doushantuo Formation，Yangtze Gorges[J]. Acta
Palaeontological Sinica，1994，33（4）：391 403.
[13] 王自强，高林志，尹崇玉. 峡东地区震旦系等时层
序地层格架的建立[J]. 中国区域地质，2001，20（4）：
368 376.
WANG Ziqiang，GAO Linzhi，YIN Chongyu. Establishment
of the Sinian isochronous sequence stratigraphic
framework in the eastern Yangtze Gorges Area[J]. Regional
Geology of China，2001，20（4）：368 376.
[14] 王自强，高林志，尹崇玉. 峡东地区震旦系层型剖面的
界定与层序划分[J]. 地质论评，2001，47（5）：449 457.
WANG Ziqiang，GAO Linzhi，YIN Chongyu. Ascertainment
and stratigraphic division of the Sinian stratotype
section[J]. Geological Review，2001，47（5）：449 457.
[15] 密文天，林丽，庞艳春，等. 湖北宜昌白果园陡山沱
组层序地层及磷块岩成因研究[J]. 沉积学报，2010，
28（3）：471 478.
MI Wentian，LIN Li，PANG Yanchun，et al. The sequence
stratigraphy and genesis of phosphorites of Doushantuo
Formation at Baiguoyuan，Yichang，Hubei[J]. Acta Sedimentologica
Sinica，2010，28（3）：471 478.
[16] 郑文忠，东野脉兴. 鄂西陡山沱组磷块岩矿层划分对
比及成矿规律[J]. 矿物岩石，1994，14（3）：89 95.
ZHENG Wenzhong，DONGYE Maixing. Division，correlation
and minerogenerating rule of the phosphorusm ineral
beds of Doushantuo Formation in western Hubei[J].
Journal of Mineralogy and Petrology，1994，14（3）：
89 95.
[17] 柳永清，尹崇玉，高林志，等. 峡东震旦系层型剖面沉
积相研究[J]. 地质评论，2003，49（2）：187 194.
LIU Yongqing，YIN Chongyu，GAO Linzhi，et al. Advances
in the study of sedimentary facies of the Sinian candidate
stratotype in the eastern areas of the Three Gorges，
Hubei[J]. Geological Review，2003，49（2）：187 194.
[18] 张琴，刘洪林，拜文华，等. 渝东南地区龙马溪组页
岩含气量及其主控因素分析[J]. 天然气工业，2013，
33（5）：35 39.
ZHANG Qin，LIU Honglin，BAI Wenhua，et al. Shale
gas content and its main controlling factors in Longmaxi
shales in southeastern Chongqing[J]. Natural Gas Industry，
2013，33（5）：35 39.
[19] 蒲泊伶，董大忠，耳闯，等. 川南地区龙马溪组页岩有
利储层发育特征及其影响因素[J]. 天然气工业，2013，
33（12）：41 47.
PU Boling，DONG Dazhong，ER Chuang，et al. Favorable
reservoir characteristics of the Longmaxi shale in the
Southern Sichuan Basin and their influencing factors[J].
Natural Gas Industry，2013，33（12）：41 47.
[20] 王兴志，李宜真，杜洋，等. 四川盆地下志留统龙马溪
组底部界线研究[J]. 西南石油大学学报（自然科学版），
2014，36（1）：45 50.
WANG Xingzhi，LI Yizhen，DU Yang，et al. Study
on Longmaxi Formation bottom boundary in Sichuan
Basin[J]. Journal of Southwest Petroleum University（Science
& Technology Edition），2014，36（1）：45 50．
[21] 武景淑，于炳松，李玉喜. 渝东南渝页1 井页岩气吸附
能力及其主控因素[J]. 西南石油大学学报（自然科学
版），2012，34（4）：40 48.
WU Jingshu，YU Bingsong，LI Yuxi. Adsorption capacity
of shale gas and controlling factors from the Well Yuye1
at the southeast of Chongqing[J]. Journal of Southwest
Petroleum University（Science & Technology Edition），
2012，34（4）：40 48.
[22] 侯读杰，包书景，毛小平，等. 页岩气资源潜力评价的
几个关键问题讨论[J]. 地球科学与环境学报，2012，
34（3）：7 16.
HOU Dujie，BAO Shujing，MAO Xiaoping，et al. Discussion
on the key issues of resource potential evaluation for
shale gas[J]. Journal of Earth Sciences and Environment，
2012，34（3）：7 16.
[23] 陈寿铭，尹崇玉，刘鹏举，等. 湖北宜昌樟村坪埃迪卡
拉系陡山沱组硅磷质结核中的微体化石[J]. 地质学报，
2010，84（1）：70 73.
CHEN Shouming，YIN Chongyu，LIU Pengju，et al.
Microfossil assemblage from chert nodules of the ediacaran
Doushantuo Formationin Zhangcunping，northern
Yichang，south China[J]. Acta Geologica Sinica，2010，
84（1）：70 73.
[24] 邢裕盛，尹崇玉，高林志. 震旦系的范畴、时限及内部
划分[J]. 现代地质，1999，13（2）：202–204.
XING Yusheng，YIN Chongyu，GAO Linzhi. The category，
time limit and internal of the Sinian[J]. Geoscience，
1999，13（2）：202 204.
[25] 唐天福，薛耀松，俞从流. 中国南方晚震旦世沉积
相及磷块岩的时空分布[J]. 沉积学报，1987，5（3）：
113 124.
TANG Tianfu，XUE Yaosong，YU Congliu. The temporal
and spatial distribution of sedimentary facies and phosphate
rock from the upper Sinian[J]. Acta Sedimentologica
Sinica，1987，5（3）：113 124.
[26] 李忠雄，陆永潮，王剑，等. 中扬子地区晚震旦世早
寒武世沉积特征及岩相古地理[J]. 古地理学报，2004，
6（2）：151 162.
LI Zhongxiong，LU Yongchao，WANG Jian，et al.
Sementary characteristics and lithofacies palaeogeography
of the Late Sinian and Early Cambrian in middle
Yangtze region[J]. Journal of Palaeogeography，2004，
6（2）：151 162.
[27] 李有禹. 湖南大庸慈利一带下寒武统黑色页岩中海底
喷流沉积硅岩的地质特征[J]. 岩石学报，1997，13（1）：
121 126.
LI Youyu. The Geological Characteristics of Sea-floor
Exhalation Sedimentary Chert in Lower Cambrian black
shales in Dayong-Cili area，Hunan Province[J]. Acta
Petrologica Sinica，1997，13（1）：121 126．

Sedimentary Characteristics and Evolution of the Upper Sinian#br# Doushantuo Formation in the North of Middle Yangtze Area

PDF (PC)

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 15

Recommended Articles

Metrics

Comments

[1]	BAI Xiaoliang, YANG Yueming, WEN Long, LUO Bing, HONG Haitao. Sedimentary Facies Distribution and Exploration Significance of the Middle Permian Qixia Formation in the Sichuan Basin [J]. 西南石油大学学报(自然科学版), 2020, 42(5): 13-24.
[2]	WANG Weidong, PENG Jun, XIA Qingsong, DUAN Guanyi, SUN Enhui. Major Controlling Factors and a Method for Predicting Bioclastic Limestone Reservoirs in Da'anzhai, Northern Sichuan [J]. 西南石油大学学报(自然科学版), 2020, 42(4): 13-21.
[3]	Lei Xiao1, Hu Yu2, Liang Wenfeng1, Liao Jijia2*, Liao Mingguang2. A Study on Sedimentary Facies of Oil Group I in Member 2 of Zhujiang Formation in Wenchang 19-1 Oilfield [J]. 西南石油大学学报(自然科学版), 2015, 37(4): 1-12.
[4]	Liu Qinqin1，2*, Huang Chuanyan2，3, Jin Siding2，3, Liu Entao2，3, Xia Cunyin4. Activity Characteristics of Meitai Fault of Fushan Depression and its Controlling on Sedimentation [J]. 西南石油大学学报(自然科学版), 2015, 37(4): 51-59.
[5]	Shi Shi1*, Gao Lixiang2, Liu Lili3, Gu Jiangrui1, Bi Mingwei2. Geological Modeling of Effective Sandstone Reservoir of the Su-6 Infilling Drilling Pilot in Sulige Gas Field [J]. 西南石油大学学报(自然科学版), 2015, 37(1): 44-50.
[6]	Zhang Ting1, Wang Qiang1, Liu Bin2. Sedimentary Facies and Its Lateral Distribution of the Middle-lower Jurassic in Amu Darya Right Bank Area [J]. 西南石油大学学报(自然科学版), 2014, 36(6): 27-38.
[7]	Yang Wei1，2, Hu Mingyi1，2, Gao Yan3. Sequence Stratigraphy and Evolution of Sedimentary Facies of Upper Perma in Jiannan Area [J]. 西南石油大学学报(自然科学版), 2014, 36(2): 24-34.
[8]	Shan Jingfu1，2, Chen Xinxin2, Le Jianghua3, Ge Daiwei2, Feng Guangye4. Sedimentary Facies Analysis in Tongbomiao Formation of Tarbell Depression [J]. 西南石油大学学报(自然科学版), 2013, 35(3): 1-8.
[9]	Ning Zhengfu;Li Dongyang;Cheng Linsong;. Prediction of Favorable Area of Chang 6 and Chang 4+5 Reservoir FromHujianshan Area [J]. 西南石油大学学报(自然科学版), 2012, 34(3): 33-40.
[10]	MA Xiao-juan ZHANG Zhong-min CHEN Zhan-kun. Stratigraphic Sequence and Sedimentary Facies of Kepingtage Formation in the Silurian at the South Area of Tahe Oilfield [J]. 西南石油大学学报(自然科学版), 2011, 33(3): 35-40.
[11]	CHU Cheng-lin LIN Chang-song ZHU yong-feng LIU Jing-yanRUI Zhi-feng. STUDY ON THE SEQUENCE STRATIGRAPHY AND DEPOSITIONAL SYSTEM OF DONGHE SANDSTONE IN TABEI UPLIFT [J]. 西南石油大学学报(自然科学版), 2011, 33(1): 15-20.
[12]	XU Guo-sheng;WANG De-bin;WANG Qing-peng;ZHOU Lian-de;ZHANG Rui. SEDIMENTARY MICROFACIES FEATURE AND THE RESERVOIR PERMEABILITY UNITS IN CARBONIFEROUS，SHAGUANPING，EASTERN SICHUAN [J]. 西南石油大学学报(自然科学版), 2010, 32 (1): 170-174.
[13]	WANG Dai-liua;b;a WANG Jiaoa;b. THE RECOGNITION AND APPLICATION OF LACUSTRINE FACIES IN GUANTAO FORMATION OF GUDAO OILFIELD [J]. 西南石油大学学报(自然科学版), 2009, 31(2): 41-44.
[14]	FAN Chun-hua;WANG Ying-min;CHEN Zhen-yan ZHANG Wen-ming;. SEQUENCE STRATIGRAPHY AND SEDIMENTARY FACIES OF THE SHA 3 LOWER SUBINTERVAL IN CHENJIA DEPRESSION [J]. 西南石油大学学报(自然科学版), 2009, 31(2): 31-35.
[15]	LUO Bing ZOU Juan TANG Qing-song DING Xiong HUANG Yong-bin. RERECOGNITION OF SEDIMENTARY FACIES OF THE JIA 2 MEMBER IN MOXI GAS FIELD [J]. 西南石油大学学报(自然科学版), 2008, 30(6): 35-39.