Distribution of heavy mineral assemblages in Wendeng nearshore waters and their implications for sedimentary dynamic environment

ZHANG Lianjie; HU Rijun; ZHU Longhai; ZHANG Pan

doi:10.16562/j.cnki.0256-1492.2018.01.013

Marine Geology & Quaternary Geology > 2018 > 38(1): 127-138. > DOI: 10.16562/j.cnki.0256-1492.2018.01.013

ZHANG Lianjie, HU Rijun, ZHU Longhai, ZHANG Pan. Distribution of heavy mineral assemblages in Wendeng nearshore waters and their implications for sedimentary dynamic environment[J]. Marine Geology & Quaternary Geology, 2018, 38(1): 127-138. DOI: 10.16562/j.cnki.0256-1492.2018.01.013

Citation:

PDF (8890 KB)

Distribution of heavy mineral assemblages in Wendeng nearshore waters and their implications for sedimentary dynamic environment

1.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Ocean University of China, Qingdao 266100, China

More Information

Received Date: February 21, 2017
Revised Date: June 07, 2017

Graphical Abstract

Abstract

Abstract

97 samples of the heavy minerals of the surface sediments in the Wendeng nearshore waters were separated and identified. The combination and distribution of heavy minerals were studied by means of correlation analysis, Q - type cluster analysis and other mathematical statistics methods. Heavy mineral provinces are established based on the results. Combined with the grain size characteristics of the sediments, we studied sedimentary source and dynamic environment of the area and the shrinkage of Wuleidao Bay. Results show that there are 4 assemblages of heavy minerals, i.e. the biotite-muscovite-weathered mica-chlorite assemblage, ilmenite-magnetite-limonite-zircon-garnet assemblage, augite-hypersthene-diopside—tourmaline assemblage and hornblende—epidote assemblage. And there are five heavy mineral provinces in the study area. The provenance and sedimentary dynamic environment of each mineral province are quite different. Adequate sediment supply and dynamic environment lead to the siltation of Wuleidao Bay, and it will continue to shrink in the future.
- heavy mineral assemblages,
- partition,
- provenance,
- sedimentary dynamic environment,
- Wendeng nearshore waters

FullText(HTML)

References (22)

References

[1]	王利波, 李军, 赵京涛, 等.辽东湾表层沉积物碎屑矿物组合分布及其对物源和沉积物扩散的指示意义[J].海洋学报, 2014, 36(2): 66-74. http://d.old.wanfangdata.com.cn/Periodical/hyxb201402007 WANG Libo, LI Jun, ZHAO Jingtao, et al. Detrital mineral assemblages and distributions as indicators of provenance and dispersal pattern in surface sediments from Liaodong Bay, Bohai Sea[J]. Acta Oceanologica Sinica, 2014, 36(2): 66-74. http://d.old.wanfangdata.com.cn/Periodical/hyxb201402007
[2]	Winkler W, Slaczka A. Sediment dispersal and provenance in the Silesian, Dukla and Magura flysch nappes (Outer Carpathians, Poland)[J]. Geologische Rundschau, 1992, 81(2): 371-382. doi: 10.1007/BF01828604
[3]	Diekmann B, Kuhn G. Provenance and dispersal of glacial-marine surface sediments in the Weddell Sea and adjoining areas, Antarctica: ice-rafting versus current transport[J]. Marine Geology, 1999, 158(1-4): 209-231. doi: 10.1016/S0025-3227(98)00165-0
[4]	Ehrmann W, Polozek K. The heavy mineral record in the Pliocene to Quaternary sediments of the CIROS-2 drill core, McMurdo Sound, Antarctica[J]. Sedimentary Geology, 1999, 128(3): 223-244. doi: 10.1016-S0037-0738(99)00071-8/
[5]	金秉福, 林振宏, 杨群慧, 等.沉积矿物学在陆缘海环境分析中的应用[J].海洋地质与第四纪地质, 2002, 22(3): 113-118. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200203021.htm JIN Bingfu, LIN Zhenghong, YANG Qunhui, et al. Application of sedimentary mineralogy to the environmental analysis in marginal seas[J]. Marine Geology &Quaternary Geology, 2002, 22(3): 113-118. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200203021.htm
[6]	Bayhan E, Ergin M, Temel A, et al. Sedimentology and mineralogy of surficial bottom deposit s from the Aegean-Canakkale-Marmara transition (Eastern Mediterranean): effects of marine and terrestrial factors[J]. Marine Geology, 2001, 175(1-4): 297-315. doi: 10.1016/S0025-3227(01)00142-6
[7]	Schafer J, Doerr W. Heavy-mineral analysis and typology of detrital zircons: A new approach to provenance study (Saxothuringian Flysch, Germany)[J]. Journal of Sedimentary Research, 1997, 67(3): 451-461.
[8]	黎广钊, 梁文, 刘敬合.从沉积物中重矿物动力分区论钦州湾泥沙来源及运移趋势[J].海洋通报, 2002, 21(5): 61-68. doi: 10.3969/j.issn.1001-6392.2002.05.009 LI Guangzhao, LIANG Wen, LIU Jinghe. Discussion on the source and transport tendency of silt in the Qinzhou bay in terms of the dynamic partition zones of heavy minerals in the sediments[J]. Marine Science Bulletin, 2002, 21(5): 61-68. doi: 10.3969/j.issn.1001-6392.2002.05.009
[9]	章伟艳, 张霄宇, 金海燕, 等.长江口-杭州湾及其邻近海域沉积动力环境及物源分析[J].地理学报. 2013, 68(5): 640-650. http://www.cnki.com.cn/Article/CJFDTotal-DLXB201305009.htm ZHANG Weiyan, ZHANG Xiaoyu, JIN Haiyan, et al. Dynamic sedimentary environment and the provenance characteristics in Yangtze River Estuary- Hangzhou Bay and its adjacent waters[J]. Acta Geographica Sinica, 2013, 68(5): 640-650. http://www.cnki.com.cn/Article/CJFDTotal-DLXB201305009.htm
[10]	王益民.文登近岸海域沉积物运移及控制因素研究[D].中国海洋大学硕士学位论文, 2014. http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=D547956 WANG Yimin. Research on sediment transport and control factors of Wendeng offshore area[D]. Master's Thesis of Ocean University of China, 2014. http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=D547956
[11]	冯秀丽, 隋倩倩, 林霖, 等.威海靖海湾港区张家埠新港建设对泥沙冲淤影响预测分析[J].海洋科学, 2011(3): 72-76. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hykx201103013 FENG Xiuli, SUI Qianqian, LIN Lin, et al. Prediction of sediment souring and depositing driven by Zhangjiabu new port construction at Jinghai bay at Weihai[J]. Marine Sciences, 2011(3): 72-76. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hykx201103013
[12]	李广雪, 宫立新, 杨继超, 等.山东滨海沙滩侵蚀状态与保护对策[J].海洋地质与第四纪地质, 2013, 33(5): 35-46. http://xueshu.baidu.com/s?wd=paperuri%3A%2867771c15f38f15735548001cbad34154%29&filter=sc_long_sign&tn=SE_xueshusource_2kduw22v&sc_vurl=http%3A%2F%2Fwww.cnki.com.cn%2FArticle%2FCJFDTotal-HYDZ201305007.htm&ie=utf-8&sc_us=11169160676130128982 LI Guangxue, GONG Lixin, YANG Jichao, et al. Beach erosion along the coast of Shandong Province and protection countermeasures[J]. Marine Geology and Quaternary Geology, 2013, 33(5): 35-46. http://xueshu.baidu.com/s?wd=paperuri%3A%2867771c15f38f15735548001cbad34154%29&filter=sc_long_sign&tn=SE_xueshusource_2kduw22v&sc_vurl=http%3A%2F%2Fwww.cnki.com.cn%2FArticle%2FCJFDTotal-HYDZ201305007.htm&ie=utf-8&sc_us=11169160676130128982
[13]	Folk R L, Andrews P B, Lewis D W. Detrital sedimentary rock classification and nomenclature for use in New Zealand[J]. New Zealand Journal of Geology and Geophysics, 1970, 13(4): 937-968. doi: 10.1080/00288306.1970.10418211
[14]	McManus J. Grain size determination and interpretation[M]//Tucker M.Techniques in Sedimentology.Oxford, UK: Blackwell Scientific Publications, 1988: 63-85.
[15]	周艳芝.波浪作用下海滩沉积物的动力学行为--以青岛仰口湾海水浴场为例[D].中国海洋大学硕士学位论文, 2010. http://cdmd.cnki.com.cn/Article/CDMD-10423-1011027428.htm ZHOU Yanzhi. Dynamics behavior of beach sediment under wave action-A case study of Yangkoubay[D]. Master's Thesis of Ocean University of China, 2010. http://cdmd.cnki.com.cn/Article/CDMD-10423-1011027428.htm
[16]	赵鹏大.矿床统计预测[M].北京:地质出版社, 1983: 2-15. ZHAO Pengda. Deposit Statistical Forecasting[M]. Beijing: Geological Publishing House, 1983: 2-15.
[17]	Gao S, Collins M B. Analysis of grain size trends, for defining sediment transport pathways in marine environments[J]. Journal of Coastal Research, 1994, 10(1): 70-78. https://www.researchgate.net/publication/279558838_Analysis_of_grain_size_trends_for_defining_sediment_transport_pathways_in_marine_environments
[18]	程鹏, 高抒.北黄海西部海底沉积物的粒度特征和净输运趋势[J].海洋与湖沼, 2000, 31(6): 604-615. doi: 10.3321/j.issn:0029-814X.2000.06.004 CHENG Peng, GAO Shu. Net sediment transport patterns over the northwestern yellow sea, based upon grain size trend analysis[J]. Oceanologia et Limnologia Sinica, 2000, 31(6): 604-615. doi: 10.3321/j.issn:0029-814X.2000.06.004
[19]	赵红格, 刘池洋.物源分析方法及研究进展[J].沉积学报, 2003, 21(3): 409-415. doi: 10.3969/j.issn.1000-0550.2003.03.007 ZHAO Hongge, LIU Chiyang. Approaches and prospects of provenance analysis[J]. Acta Sedimentologica Sinica, 2003, 21(3): 409-415. doi: 10.3969/j.issn.1000-0550.2003.03.007
[20]	施振生, 王秀芹, 吴长江.四川盆地上三叠统须家河组重矿物特征及物源区意义[J].天然气地球科学, 2011, 22(4): 618-627. http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201104008 SHI Zhensheng, WANG Xiuqin, WU Changjiang. The heavy minerals and provenances of the upper Triassic Xujiahe formation in Sichuan basin[J]. Natural Gas Geoscience, 2011, 22(4): 618-627. http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201104008
[21]	沈丽琪.沉积岩重矿物研究中的几个重要概念及其应用[J].中国科学B辑, 1985(1): 70-78. http://www.cnki.com.cn/Article/CJFDTotal-JBXK198501010.htm SHEN Liqi. Several important concepts and their application in the study of heavy mineral sediments[J]. Science in China Series B, 1985(1): 70-78. http://www.cnki.com.cn/Article/CJFDTotal-JBXK198501010.htm
[22]	刘群明, 陈开远, 王键, 等.柴达木盆地三湖坳陷第四系重矿物物源分析[J].现代地质, 2011, 25(2): 315-321. doi: 10.3969/j.issn.1000-8527.2011.02.015 LIU Qunming, CHEN Kaiyuan, WANG Jian, et al. The provenance analysis of the Quaternary heavy minerals in the Sanhu depression, Qaidambasin[J]. Geoscience, 2011, 25(2): 315-321. doi: 10.3969/j.issn.1000-8527.2011.02.015