峨眉山玄武岩作为长江上游特征源岩对三峡贯通的指示

杨建; 李长安; N'dji ditJacques Dembele; 江华军

doi:10.3799/dqkx.2014.041

Volume 39 Issue 4

Apr. 2014

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2014 > 39(4): 431-442

Yang Jian, Li Chang'an, N'dji dit Jacques Dembele, Jiang Huajun, 2014. Emeishan Basalts as Provenance Indicators: Implications for Formation of the Three Gorges. Earth Science, 39(4): 431-442. doi: 10.3799/dqkx.2014.041

Citation:

Yang Jian, Li Chang'an, N'dji dit Jacques Dembele, Jiang Huajun, 2014. Emeishan Basalts as Provenance Indicators: Implications for Formation of the Three Gorges. Earth Science, 39(4): 431-442. doi: 10.3799/dqkx.2014.041

Citation:

PDF( 2922 KB)

Emeishan Basalts as Provenance Indicators: Implications for Formation of the Three Gorges

doi: 10.3799/dqkx.2014.041

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

Received Date: 2013-08-16
Publish Date: 2014-04-15

Abstract

Abstract

The Emeishan basalts are typical rocks of the Yangtze River basin because of their unique origin, the broad distribution and simplicity of identification, which can be used as an indicator of tracing the source of the upstream Yangtze sediments after cutting of the Three Gorges. The gravel and debris (between 1-2 mm) of basalts in the sediments of the middle and upper reaches of the Yangtze terraces(above Fuling City) and the Quaternary sediments of the Zhoulao core in the Jianghan Plain are mainly studied in the article. The gravels of the lithic basalts are abundant in the floodplain sediments and the terrace deposits along the upper reach of the river (upstream of Fuling City), and are rare along the downstream of the Three Gorges. The basalt debris are very common on the terraces of the upper reach of the Yangtze River, and are also evaluated by the loose sediments of the Zhoulao core. These lithic debris were identified as the Emeishan basalts by LA-ICP-MS and appear at the core depth of 156 m (up). This line of change (156 m depth) dated of about 1.7 Ma attests a provenance change. Meanwhile, a wide drainage basin similar as today's dimension of the Yangtze River had formed and the Three Gorges had formed around 1.7 Ma.
- Emeishan basalts,
- Jianghan Plain,
- Quaternary,
- sediments,
- trace elements,
- source tracing,
- evolution of the Yangtze River

FullText(HTML)

References(49)

References

Chen, H.H., Ma, Z.L., 1987. Lower Pleistocene Series in Jianghan Plain. Earth Science—Journal of Wuhan College of Geology, 12(2): 129-135 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX198702003.htm

Clark, M.K., Schoenbohm, L.M., Royden, L.H., et al., 2004. Surface Uplift, Tectonics, and Erosion of Eastern Tibet from Large-Scale Drainage Patterns. Tectonics, 23(1): 1-20. doi: 10.1029/2002TC001402

Fan, D.D., Li, C.X., Yokoyama, K., et al., 2004. Monazite Age Spectra in the Late Cenozoic Strata of the Changjiang Delta and Its Implication on the Changjiang Run-Through Time. Science in China (Ser. D), 34(11): 1015-1022 (in Chinese). http://d.wanfangdata.com.cn/Periodical_NSTL_QKJJ028318266.aspx

Hu, Z.C., Gao, S., Liu, Y.S., et al., 2008. Signal Enhancement in Laser Ablation ICP-MS by Addition of Nitrogen in the Central Channel Gas. Journal of Analytical Atomic Spectrometry, 23(8): 1093-1101. doi: 10.1039/B804760J

Hubei Bureau of Geology and Mineral Resources, 1991. Regional Geology of Hubei Province. Geological Publishing House, Beijing, 343-400(in Chinese).

Kang, C.G., Li, C.A., Wang, J.T., et al., 2009. Heavy Mineral Characteristics of Sediments in Jianghan Plain and Its Indication to the Forming of the Three Gorges. Earth Science—Journal of China University of Geosciences, 34(3): 419-427 (in Chinese with English abstract). doi: 10.3799/dqkx.2009.047

Liu, Y.S., Gao, S., Hu, Z.C., et al., 2010. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths. Journal of Petrology, 51(1-2): 537-571. doi: 10.1093/petrology/egp082

Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1-2): 34-43. doi: 10.1016/j.chemgeo.2008.08.004

Lü, Q.R., 1992. Mineral Characteristics of Fine-Grain Sediment and Its Sedimentary Differentiation in Changjiang Estuary. Shanghai Geology, 43(3): 18-25, 40 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SHAD199203002.htm

Ma, Y.F., Li, C.A., Wang, Q.L., et al., 2007. Statistics of Gravels from a Bore in Zhoulao Town, Jianghan Plain and Its Relationship with Cut-Through of the Yangtze Three Gorges, China. Geological Science and Technology Information, 26(2): 40-44 (in Chinese with English Abstract). http://www.cqvip.com/QK/93477A/20072/24094697.html

Pearce, J.A., Cann, J.R., 1973. Tectonic Setting of Basic Volcanic Rocks Investigated Using Trace Element Analyses. Earth and Planetary Science Letters, 19(2): 290-300. doi: 10.1016/0012-821X(73)90129-5

Richardson, N.J., Densmore, A.L., Seward, D., et al., 2010. Did Incision of the Three Gorges Begin in the Eocene?Geology, 38(6): 551-554. doi: 10.11/G30527.1

Song, X.Y., Hou, Z.Q., Wang, Y.L., et al., 2002. The Mantle Plume Features of Emeishan Basalts. Journal of Mineralogy and Petrology, 22(4): 27-32 (in Chinese with English abstract). http://www.researchgate.net/publication/292927725_The_mantle_plume_features_of_Emeishan_basalts

Sun, B.Y., 1990. Detrital Mineral Assemblages in the Huanghe, Changjiang and Zhujiang River Delta Sediments. Marine Geology & Quaternary Geology, 10(3): 23-34(in Chinese with English abstract). http://www.researchgate.net/publication/285012617_Detrital_mineral_assemblages_in_the_Huanghe_Changjiang_and_Zhujiang_River_delta_sediments

Sun, X.L., Li, C.A., 2010. ⁴⁰Ar-³⁹Ar Age Tracing of Detrital Muscovites and Its Application in Yangtze River Running-Through Time. Geological Science and Technology Information, 29(6): 121-127 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ201006021.htm

Wang, J.T., Li, C.A., Yang, Y., et al., 2010. Detrital Zircon Geochronology and Provenance of Core Sediments in Zhoulao Town, Jianghan Plain, China. Journal of Earth Science, 21(3): 257-271. doi: 10.1007/S12583-010-0090-4

Wang, L.C., Chen, X.L., Chu, T.Q., 1997. A Contrast Analysis on the Loads Character of the Changjiang River and the Yellow River. Geographical Research, 16(4): 71-79 (in Chinese with English abstract).

Wang, Z.B., Yang, S.Y., Li, P., et al., 2006. Detrital Mineral Compositions of the Changjiang River Sediments and Their Tracing Implications. Acta Sedimentologica Sinica, 24(4): 570-578 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-CJXB200604014.htm

Xiang, F., Zhu, L.D., Wang, C.S., et al., 2006. Character of Basaltic Gravels in Quaternary Sediments in Yichang Area and Its Relationship with Formation of Yangtze Three Gorges. Journal of Earth Sciences and Environment, 28(2): 6-10, 24 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XAGX200602001.htm

Xiao, L., Xu, Y.G., Chuang, S.L., et al., 2003. Chemostratigraphic Correlation of Upper Permian Lava Succession from Yunnan Province, China: Extent of the Emeishan Large Igneous Province. International Geology Review, 45: 753-766. doi: 10.2747/0020-6814.45.8.753

Yan, Q.R., Hanson, A.D., Wang, Z.Q., et al., 2004. Geochemistry and Tectonic Setting of the Bikou Volcanic Terrane on the Northern Margin of the Yangtze Plate. Acta Petrologica et Mineralogica, 23(1): 1-11 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200401000.htm

Yang, D.Y., 1988. The Origin and Evolution of the Three Gorges of the Changjiang Yangtze River. Journal of Nanjing University (Natural Sciences Edition), 24(3): 466-474 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-NJDZ198803009.htm

Yang, S.Y., 2006. Advances in Sedimentary Geochemistry and Tracing Applications of Asian Rivers. Advances in Earth Science, 21(6): 648-655 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXJZ200606013.htm

Zhang, C.L., Zhou, D.W., Liu, Y.Y., 1999. Geochemistry of Basic Dykes in Wudangshan Block and Their Tectonic Significance. Geochimica, 28(2): 126-135(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX902.002.htm

Zhang, H.X., Xu, Z.F., Ma, Y.J., et al., 2001. Geochemical Features and Origin of Continental Flood Basalts. Earth Science—Journal of China University of Geosciences, 26(3): 261-268 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200103007.htm

Zhang, Y.F., Li, C.A., Wang, Q.L., et al., 2008. Magnetism Parameters Characteristics of Drilling Deposits in Jianghan Plain and Indication for Forming of the Yangtze River Three Gorges. Chinese Science Bulletin, 53(5): 577-582 (in Chinese). doi: 10.1360/csb2008-53-5-577

Zhang, Y.X., Luo, Y.N., Yang, C.X., 1988. Panxi Rift. Geological Publishing House, Beijing(in Chinese)

Zheng, H.B., Jia, D., Chen, J., et al., 2013. Did Incision of the Three Gorges Begin in the Eocene? COMMENT. Geology, 39 (5): 244-245. doi: 10.1130/G31944C.1

Zheng, H.F., Xie, H.S., Guo, J., 1998. Reliability of Trace Element Ratios in the Study of the Composition of Magma Source Region: Experimental Study on Basalt Melting. Acta Mineralogica Sinica, 18(4): 541-545(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWXB199804020.htm

陈华慧, 马祖陆, 1987. 江汉平原下更新统. 地球科学——武汉地质学院学报, 12(2): 129-135. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198702003.htm

范代读, 李从先, Yokoyama, K., 等, 2004. 长江三角洲晚新生代地层独居石年龄谱与长江贯通时间研究. 中国科学(D辑), 34(11): 1015-1022. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200411003.htm

湖北省地质矿产局, 1991. 湖北省区域地质志. 北京: 地质出版社, 343-400.

康春国, 李长安, 王节涛, 等, 2009. 江汉平原沉积物重矿物特征及其对三峡贯通的指示. 地球科学——中国地质大学学报, 34(3): 419-427. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200903006.htm

吕全荣, 1992. 长江口细颗粒沉积物的矿物特征和沉积分异. 上海地质, 43(3): 18-25, 40. https://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199203002.htm

马永法, 李长安, 王秋良, 等, 2007. 江汉平原周老镇钻孔砾石统计及其与长江三峡贯通的关系. 地质科技情报, 26(2): 40-44. doi: 10.3969/j.issn.1000-7849.2007.02.008

宋谢炎, 侯增谦, 汪云亮, 等, 2002. 峨眉山玄武岩的地慢热柱成因. 矿物岩石, 22(4): 27-32. doi: 10.3969/j.issn.1001-6872.2002.04.006

孙白云, 1990. 黄河、长江和珠江三角洲沉积物中碎屑矿物的组合特征. 海洋地质与第四纪地质, 10(3): 23-34. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ199003002.htm

孙习林, 李长安, 2010. 碎屑白云母⁴⁰Ar-³⁹Ar示踪及在长江贯通研究中的应用探讨. 地质科技情报, 29(6): 121-127. doi: 10.3969/j.issn.1000-7849.2010.06.021

王腊春, 陈晓玲, 储同庆, 1997. 黄河、长江泥沙特性对比分析. 地理研究, 16(4): 71-79. https://www.cnki.com.cn/Article/CJFDTOTAL-DLYJ704.009.htm

王中波, 杨守业, 李萍, 等, 2006. 长江水系沉积物碎屑矿物组成及其示踪意义. 沉积学报, 24(4): 570-578. doi: 10.3969/j.issn.1000-0550.2006.04.015

向芳, 朱利东, 王成善, 等, 2006. 宜昌地区第四纪沉积物中玄武岩砾石特征及其与长江三峡贯通的关系. 地球科学与环境学报, 28(2): 6-10, 24. doi: 10.3969/j.issn.1672-6561.2006.02.002

闫全人, Hanson, A.D., 王宗起, 等, 2004. 扬子板块北缘碧口群火山岩的地球化学特征及其构造环境. 岩石矿物学杂志, 23(1): 1-11. doi: 10.3969/j.issn.1000-6524.2004.01.001

杨达源, 1988. 长江三峡的起源与演变. 南京大学学报(自然科学版), 24(3): 466-474. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ198803009.htm

杨守业, 2006. 亚洲主要河流的沉积地球化学示踪研究进展. 地球科学进展, 21(6): 648-655. doi: 10.3321/j.issn:1001-8166.2006.06.013

张成立, 周鼎武, 刘颖宇, 1999. 武当山地块基性岩墙群地球化学研究及其大地构造意义. 地球化学, 28(2): 126-135. doi: 10.3321/j.issn:0379-1726.1999.02.003

张鸿翔, 徐志方, 马英军, 等, 2001. 大陆溢流玄武岩的地球化学特征及起源. 地球科学——中国地质大学学报, 26(3): 261-268. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200103007.htm

张玉芬, 李长安, 王秋良, 等, 2008. 江汉平原沉积物磁学特征及对长江三峡贯通的指示. 科学通报, 53(5): 577-582. doi: 10.3321/j.issn:0023-074X.2008.05.013

张云湘, 骆耀南, 杨崇喜, 1988. 攀西裂谷. 北京: 地质出版社.

郑海飞, 谢鸿森, 郭捷, 1998. 微量元素比值研究岩浆源区成分的可靠性: 玄武岩熔融实验研究. 矿物学报, 18(4): 541-545. doi: 10.3321/j.issn:1000-4734.1998.04.021

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(5) / Tables(3)

Get Citation

PDF

XML

Article views (3617) PDF downloads(467)

Emeishan Basalts as Provenance Indicators: Implications for Formation of the Three Gorges

doi: 10.3799/dqkx.2014.041

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content