Research on the Sedimentary and Paleoclimate Environment of the Xiaoheba Formation in Southeastern Sichuan Based on the Trace Elements Ratio Method

Hai-ou YANG; Chang-cheng WANG; Wen-jie LI; Hua DONG; Xiao-xing GONG

doi:10.15898/j.cnki.11-2131/td.201607200103

Rock and Mineral Analysis > 2017 > 36(3): 289-296. > DOI: 10.15898/j.cnki.11-2131/td.201607200103

Hai-ou YANG, Chang-cheng WANG, Wen-jie LI, Hua DONG, Xiao-xing GONG. Research on the Sedimentary and Paleoclimate Environment of the Xiaoheba Formation in Southeastern Sichuan Based on the Trace Elements Ratio Method[J]. Rock and Mineral Analysis, 2017, 36(3): 289-296. DOI: 10.15898/j.cnki.11-2131/td.201607200103

Citation:

PDF (1180 KB)

Research on the Sedimentary and Paleoclimate Environment of the Xiaoheba Formation in Southeastern Sichuan Based on the Trace Elements Ratio Method

1.
College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China
2.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China

More Information

Received Date: July 19, 2016
Revised Date: January 21, 2017
Accepted Date: March 19, 2017
Published Date: May 31, 2017

Abstract

Highlights
· Trace element ratio analysis can realize semi-quantitative discrimination of sedimentary environment and promote further development of quantitative study of sedimentary environment.

· Xiaoheba formation belonged to a warm and humid paleoclimate in southeast area of Sichuan Province.

· Xiaoheba formation was delta freshwater sedimentary in the southeast area of Sichuan Province.

ABSTRACT

Lower Silurian sandstone of the Xiaoheba formation in Southeastern Sichuan has a good reservoir seal combination, and an oil and gas geological condition, but the hypothesis that the sedimentary environment belongs to continental or marine sedimentary deltas remains a matter of debate. In order to solve this problem, 74 samples were collected from 9 typical sections. The elemental composition was determined by the trace element ratio method. Combined with the tectonic background and source characteristics, the sedimentary and paleoclimatic environment were discussed. X-ray Fluorescence Spectrometry (XRF) was used to analyze Ba, Mn, Sr, Cu and other trace elements, which are useful in discriminating between the sea and land facies sedimentary environment. The results show that the average Sr/Ba value is 0.2790 with the maximum of 2.31, the Mn/Fe value is 0.0093 to 0.0778, and the Sr/Ca value is 0.0005 to 0.0414, typical of freshwater delta sedimentary characteristics. The average Sr/Ba is less than 1, the average Sr/Cu is 4.8758, and more than 8.1% samples have Sr/Cu values greater than 10, reflecting the warm, moist, ancient climate environment.
- trace elements,
- Xiaoheba Formation,
- sedimentary environment,
- paleoclimate,
- X-ray Fluorescence Spectrometry

FullText(HTML)

References (22)

References

朱志军, 陈洪德.川东南地区早志留世晚期沉积特征及沉积模式分析[J].中国地质, 2012, 39(1):64-76. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201201008.htm

Zhu Z J, Chen H D.An analysis of sedimentary characteristics and model of Silurian Xiaoheba Formation in southeastern Sichuan Province[J].Geology in China, 2012, 39(1):64-76. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201201008.htm

王国茹, 陈洪德, 朱志军, 等.川东南-湘西地区志留系小河坝组砂岩稀土元素特征及其地质意义[J].成都理工大学学报, 2011, 38(1):7-14. http://www.cnki.com.cn/Article/CJFDTOTAL-SYSD201005017.htm

Wang G R, Chen H D, Zhu Z J, et al.The characteristics and geological implications of rare earth elements in sandstone of lower Silurian Xiaoheba Formation in the southeastern Sichuan-western Hunan[J].Journal of Chengdu University of Technology, 2011, 38(1):7-14. http://www.cnki.com.cn/Article/CJFDTOTAL-SYSD201005017.htm

张欣平, 张纯臣, 王大任.湘西北地区志留系泥盆系的痕迹化石[J].湖南地质, 1986, 5(2):49-61. http://www.cnki.com.cn/Article/CJFDTOTAL-HNDZ198602005.htm

Zhang X P, Zhang C C, Wang D R.The trace fossils of Silurian and Devonian systems of the northwest region, Hunan Province[J].Hunan Geology, 1986, 5(2):49-61. http://www.cnki.com.cn/Article/CJFDTOTAL-HNDZ198602005.htm

王正和, 谭钦银, 何利, 等.川东南-黔北志留系石牛栏组沉积与层序地层[J].石油与天然气地质, 2013, 34(4):499-507. doi: 10.11743/ogg20130411

Wang Z H, Tan Q Y, He L, et al.Deposition and sequence stratigraphy of the Silurian Shiniulan Formation in southeastern Sichuan-northern Guizhou Province[J].Oil & Gas Geology, 2013, 34(4):499-507. doi: 10.11743/ogg20130411

杨明太, 唐慧.能量色散X射线荧光光谱仪现状及其发展趋势[J].核电子学与探测技术, 2011, 31(12):1307-1311. doi: 10.3969/j.issn.0258-0934.2011.12.001

Yang M T, Tang H.The actualities and trend of energy dispersive X-ray fluorescence spectrometry[J].Nuclear Electronics & Detection Technology, 2011, 31(12):1307-1311. doi: 10.3969/j.issn.0258-0934.2011.12.001

杨明太.放射性核素迁移研究的现状[J].核电子学与探测技术, 2006, 26(6):1025-1028. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGAN200411001023.htm

Yang M T.Recent developments in studies for migration of radionuclides[J].Nuclear Electronics & Detection Technology, 2006, 26(6):1025-1028. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGAN200411001023.htm

吉昂.X射线荧光光谱三十年[J].岩矿测试, 2012, 31(3):383-398. http://www.ykcs.ac.cn/ykcs/ch/reader/view_abstract.aspx?file_no=20120302&flag=1

Ji A.Development of X-ray fluorescence spectrometry in the 30 years[J].Rock and Mineral Analysis, 2012, 31(3):383-398. http://www.ykcs.ac.cn/ykcs/ch/reader/view_abstract.aspx?file_no=20120302&flag=1

Andrew T, Montserrat F.Field-portable-XRF reveals the ubiquity of antimony in plastic consumer products[J].Science of the Total Environment, 2017, 584-585:982-989. doi: 10.1016/j.scitotenv.2017.01.149

孔芹, 陈磊, 汪灵.非金属矿二级标样配制及其粉末样品的XRF分析方法[J].光谱学与光谱分析, 2012, 32(5):1405-1409. http://www.cnki.com.cn/Article/CJFDTOTAL-GUAN201205067.htm

Kong Q, Chen L, Wang L.Preparation of sub-standard samples and XRF analytical method of powder non-metallic minerals[J].Spectroscopy and Spectral Analysis, 2012, 32(5):1405-1409. http://www.cnki.com.cn/Article/CJFDTOTAL-GUAN201205067.htm

高拉凡, 王长城, 杨海欧, 等.XRF法四川盆地须家河组沉积相研究中的应用[J].光谱学与光谱分析, 2016, 36(6):1904-1909. http://www.cnki.com.cn/Article/CJFDTOTAL-GUAN201606059.htm

Gao L F, Wang C C, Yang H O, et al.Application of X-ray fluorescence spectrometry in Xujiahe Formation of Sichuan basin for the study of sedimentary facies[J].Spectroscopy and Spectral Analysis, 2016, 36(6):1904-1909. http://www.cnki.com.cn/Article/CJFDTOTAL-GUAN201606059.htm

王国平, 刘景双, 翟正丽.沼泽沉积剖面特征元素比值及其环境意义——盐碱化指标及气候干湿变化[J].地理科学, 2005, 25(3):335-339. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX200503013.htm

Wang G P, Liu J S, Zhai Z L.Ratio of elements and their implications within typical sedimentation profile in the marsh-Slinization indicators and climatic change between the arid and the humid[J].Scientia Geographica Sinica, 2005, 25(3):335-339. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX200503013.htm

熊小辉, 肖加飞.沉积环境的地球化学示踪[J].地球与环境, 2011, 39(3):405-414. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ201103021.htm

Xiong X H, Xiao J F.Geochemical indicators of sedimentary environments-A summary[J].Earth and Environment, 2011, 39(3):405-414. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ201103021.htm

金艳, 傅强.东海盆地某油气田井层沉积体系研究[J].海洋石油, 2013(4):19-23. http://www.cnki.com.cn/Article/CJFDTOTAL-HYSY201304007.htm

Jin Y, Fu Q.Study on sedimentary system of formation in Well A in and gas field of East China Sea[J].Offshore Oil, 2013(4):19-23. http://www.cnki.com.cn/Article/CJFDTOTAL-HYSY201304007.htm

朱志军, 陈洪德, 林良彪, 等.黔北-川东南志留系层序格架下的沉积体系演化特征及有利区带预测[J].地质科技情报, 2010, 29(2):24-32. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201002006.htm

Zhu Z J, Chen H D, Lin L B, et al.Depositional system evolution characteristics in the frame work of sequences of Silurian and prediction of favorable zones in the Northern Gui Zhou-Southeastern Sichuan[J].Geological Science and Technology Information, 2010, 29(2):24-32. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201002006.htm

刘刚, 周东升.微量元素分析在判别沉积环境中的应用——以江汉盆地潜江组为例[J].石油实验地质, 2007, 29(3):307-314. doi: 10.11781/sysydz200703307

Liu G, Zhou D S.Application of microelements analysis in identifying sedimentary environment-Taking Qianjiang Formation in the Jianghan basin as an example[J].Petroleum Geology & Experiment, 2007, 29(3):307-314. doi: 10.11781/sysydz200703307

钱利军, 陈洪德, 林良彪, 等.四川盆地西缘地区中侏罗统沙溪庙组地球化学特征及其环境意义[J].沉积学报, 2012, 30(6):1061-1071. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201206007.htm

Qian L J, Chen H D, Lin L B, et al.Geochemical characteristics and environmental implications of middle Jurassic Shaximiao Formation, western margin of Sichuan basin[J].Acta Sedimentologica Sinica, 2012, 30(6):1061-1071. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201206007.htm

宋明水.东营凹陷南斜坡沙四段沉积环境的地球化学特征[J].矿物岩石, 2005, 25(1):67-73. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200501013.htm

Song M S.Sedimentary environment geochemistry in the Shasi section of Southern Ramp, Dongying depression[J].Journal of Mineral Petrology, 2005, 25(1):67-73. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200501013.htm

邓平.微量元素在油气勘探中的应用[J].石油勘探与开发, 1993, 20(1):27-32. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201105020.htm

Deng P.The application of trace amount of elements in the exploration of oil and gas[J]. Petroleum Exploration and Development, 1993, 20(1):27-32. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201105020.htm

孙顺才.长江三角洲全新世沉积特征[J].海洋学报, 1981, 3(1):97-113. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198704008.htm

Sun S C.Deltaic sediments of the Changjiang Delta and its characteristics[J].Acta Oceanologica Sinica, 1981, 3(1):97-113. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198704008.htm

马光祖, 梁国立.地质样品的X射线荧光光谱分析[J].岩矿测试, 1992, 11(1-2):37-43. http://www.ykcs.ac.cn/ykcs/ch/reader/view_abstract.aspx?file_no=19920105&flag=1

Ma G Z, Liang G L.X-ray fluorescence spectrometric analysis of geological samples[J].Rock and Mineral Analysis, 1992, 11(1-2):37-43. http://www.ykcs.ac.cn/ykcs/ch/reader/view_abstract.aspx?file_no=19920105&flag=1

王随继, 黄杏珍, 妥进才, 等.泌阳凹陷核桃园组微量元素演化特征及其古气候意义[J].沉积学报, 1997, 15(1):65-70. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB701.011.htm

Wang S J, Huang X Z, Tuo J C, et al.Evolutional characteristics and their paleoclimate significance of trace elements in the Hetaoyuan Formation, Biyang depression[J].Acta Sedimentologica Sinica, 1997, 15(1):65-70. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB701.011.htm

安凤桐, 高善明, 李元芳.用微量元素分析法研究滦河三角洲沉积环境[J].海洋湖沼通报, 1982(2):24-31. http://www.cnki.com.cn/Article/CJFDTOTAL-HYFB198202004.htm

An F T, Gao S M, Li Y F.A research on depositional environment of delta by analyzed method of trace elements in Luanher River[J].Transactions of Oceanology and Limnology, 1982(2):24-31. http://www.cnki.com.cn/Article/CJFDTOTAL-HYFB198202004.htm

Supplements (0)

Cited By

Cited by

Periodical cited type(11)

1.	于秋莲，陈载林，彭明兴，张展适. 酒泉盆地胳塘沟组微量元素地球化学特征及其古环境研究. 科技创新与应用. 2025(02): 89-93 .
2.	何文祥，张梦蝶，胡勇，侯云东. 鄂尔多斯盆地西缘石炭纪羊虎沟组海岸砂坝特征与成因. 长江大学学报(自然科学版). 2024(03): 1-9 .
3.	杨晋东，于振锋，郭旭，赵瑞熙. 鄂尔多斯盆地东缘晚古生代泥岩地球化学特征及有机质富集机理. 岩矿测试. 2023(06): 1104-1119 . 本站查看
4.	郇志鹏，胡剑风，王志民，宋金鹏，莫涛，郝祥保，田盼盼，崔德育，杨敬博，李浩平，刘新宇，平忠伟. 库车坳陷古近系盐底卡层技术研究与应用. 中国石油勘探. 2022(01): 142-150 .
5.	古榕，王智闻，周华. 准噶尔南缘中段上侏罗统—下白垩统沉积古环境分析. 中国锰业. 2022(05): 11-15 .
6.	宋金鹏，郇志鹏，田盼盼，杨连刚，代俊杰，王珠峰，邱升梁. 超深致密砂岩储层特征及影响因素——以库车坳陷阳霞凹陷侏罗系为例. 断块油气田. 2021(05): 592-597 .
7.	宋金鹏，田盼盼，代俊杰，杨连刚，戴瑞瑞，郭喜阳. 塔里木盆地库车坳陷膏盐岩分布特征及油气地质意义. 断块油气田. 2021(06): 800-804 .
8.	杨威，魏国齐，李德江，刘满仓，谢武仁，金惠，沈珏红，郝翠果，王小丹. 四川盆地志留系小河坝组砂岩油气地质特征与勘探方向. 天然气地球科学. 2020(01): 1-12 .
9.	邱玉超，罗冰，夏茂龙，李亚丁，黄力，叶茂. 四川盆地志留系小河坝组海相碎屑岩勘探方向及潜力. 天然气勘探与开发. 2019(01): 1-7 .
10.	王子玉，范玉蝶，徐秋阳，李丽蓉，公维杰. 南海海域珊瑚礁元素分析试验研究. 海洋技术学报. 2019(03): 64-69 .
11.	方金梅. 福建龙海市土壤与稻米铅地球化学特征分析. 岩矿测试. 2018(03): 327-335 . 本站查看

Other cited types(9)

Get Citation

PDF

XML

Article views (1659) PDF downloads (27) Cited by(20)

Turn off MathJax

Article Contents

ABSTRACT

References

Research on the Sedimentary and Paleoclimate Environment of the Xiaoheba Formation in Southeastern Sichuan Based on the Trace Elements Ratio Method

ABSTRACT

References

Cited by

Periodical cited type(11)

Other cited types(9)

Catalog

Export File

Citation

Format

Content