Mineral compositions and characteristics of the offshore clastic sediments in Haizhou Bay, Lianyungang City

TANG Qian; YAN Yuru; ZHOU Xin; CHI Ye; OUYANG Kai; DOU Chuanwei; PING Lijiao

doi:10.16788/j.hddz.32-1865/P.2021.02.013

2021 Vol. 42, No. 2

Article Contents

Article navigation > East China Geology > 2021 > 42(2): 239-245

Next Article Previous Article

TANG Qian, YAN Yuru, ZHOU Xin, CHI Ye, OUYANG Kai, DOU Chuanwei, PING Lijiao. 2021. Mineral compositions and characteristics of the offshore clastic sediments in Haizhou Bay, Lianyungang City. East China Geology, 42(2): 239-245. doi: 10.16788/j.hddz.32-1865/P.2021.02.013

Citation:

TANG Qian, YAN Yuru, ZHOU Xin, CHI Ye, OUYANG Kai, DOU Chuanwei, PING Lijiao. 2021. Mineral compositions and characteristics of the offshore clastic sediments in Haizhou Bay, Lianyungang City. East China Geology, 42(2): 239-245. doi: 10.16788/j.hddz.32-1865/P.2021.02.013

Mineral compositions and characteristics of the offshore clastic sediments in Haizhou Bay, Lianyungang City

Institute of Geochemical Exploration and Marine Geological Survey, Jiangsu Non-ferrous Metals East China Geological Exploration Bureau, Nanjing 210007, Jiangsu, China

More Information

Corresponding author: YAN Yuru, 36928254@qq.com

Received Date: 18 January 2020

Revised Date: 06 May 2020

Publish Date: 18 August 2021

Abstract

Abstract

The characteristic indexes of stable heavy minerals can well reflect the provenance informations of sediments. The clastic sediments are collected from the rivers flowing into sea and sea areas in Haizhou Bay of Lianyungang City to analyze the mineral compositions and characteristics of offshore clastic sediments. The light minerals in the offshore sediments are mainly composed of quartz and feldspar, while the heavy minerals consist of zircon, ilmenite, epidote, hornblende, sphene and garnet. The analysis of heavy mineral characteristic indexes shows that the offshore seasand sediments are the products of estuarine-neritic environment, with the placers mainly from the granite, gneiss and eclogite of Lianyungang area, belonging to the littoral sedimentary type of river-sea interaction.
- Haizhou Bay /
- characteristic index of heavy mineral /
- provenance /
- genesis /
- littoral sedimentary deposit

FullText(HTML)

References

[1]	陈丽蓉, 徐文强, 申顺喜.东海沉积物的矿物组合及其分布特征的研究[J]. 科学通报, 1979(15):709-711. Google Scholar
[2]	王先兰, 马克俭, 陈建林, 等.东海沉积物碎屑矿物特征的研究[J]. 中国科学:地球科学, 1985, 15(5):474-482. Google Scholar
[3]	金翔龙.东海海洋地质[M]. 北京:海洋出版社, 1992:173-215. Google Scholar
[4]	王中波, 杨守业, 张志珣, 等.东海西北部陆架表层沉积物重矿物组合及其沉积环境指示[J]. 海洋学报:中文版, 2012, 34(6):114-125. Google Scholar
[5]	张凯棣, 李安春, 董江, 等.东海表层沉积物碎屑矿物组合分布特征及其物源环境指示[J]. 沉积学报, 2016, 34(5):902-909. Google Scholar
[6]	周晓静.东海陆架细颗粒沉积物组成分布特征及其物源指示[D]. 青岛:中国科学院研究生院(海洋研究所), 2009:1-146. Google Scholar
[7]	MORTON A C, HAⅡSWORTH C R. Processes controlling the composition of heavy mineral assemblages in sandstones[J]. Sedimentary Geology, 1999, 124(1/4):3-29. Google Scholar
[8]	MORTON A C, HAⅡSWORTH C. Identifying provenance-specific features of detrital heavy mineral assemblages in sandstones[J]. Sedimentary Geology, 1994, 90(3/4):241-256. Google Scholar
[9]	郑光膺.黄海第四纪地质[M]. 北京:科学出版社, 1991:112-120. Google Scholar
[10]	周莉, 赵其渊, 李巍然.山东半岛南部表层沉积物粒度分布与泥砂动态[J]. 山东海洋学院学报, 1983, 13(3):45-58. Google Scholar
[11]	李玉瑛, 沈渭铨, 章伟.鲁南沿海沉积物分布规律的研究[J]. 青岛海洋大学学报, 1997, 27(4):546-552. Google Scholar
[12]	胡邦琦.中国东部陆架海泥质沉积区的物源识别及其环境记录[D]. 青岛:中国海洋大学, 2010:1-162. Google Scholar
[13]	PETTIJOHN F J, POTTER P E, SIEVER R. Sand and Sandstone[M]. Berlin:Springer Verlag, 1987. Google Scholar
[14]	MORTON A C. Heavy minerals in provenance stu-dies[M]//ZUFFA G G. Provenance of Arenites.Dordrecht:Reidel Publishing Company, 1985:249-277. Google Scholar
[15]	HUBERT J F. A zircon-tourmaline-rutile maturity index and the interdependence of the composition of heavy mineral assemblages with the gross composition and texture of sandstones[J]. Journal of Sedimentary Research, 1962, 32(3):440-450. Google Scholar
[16]	秦蕴珊, 赵一阳, 陈丽蓉, 等.黄海地质[M]. 北京:海洋出版社, 1989:3-28. Google Scholar
[17]	沈昆, 张泽明, 孙晓明, 等.超高压变质流体的组成与演化:中国大陆科学钻探工程主孔岩心的流体包裹体初步研究[J]. 岩石学报, 2005, 21(2):489-504. Google Scholar
[18]	刘敏厚, 吴世迎, 王永吉, 等.黄海晚第四纪沉积[M]. 北京:海洋出版社, 1987:293-301. Google Scholar
[19]	杜建国.连云港地区第四纪沉积地层特征[J]. 江苏地质, 1999, 23(4):229-235. Google Scholar
[20]	中华人民共和国国土资源部.DZ/T 0208-2002砂矿(金属矿产)地质勘查规范(附录C)[S]. 北京:中国标准出版社, 2002. Google Scholar
[21]	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中重矿物特征及地质意义[J]. 成都理工大学学报:自然科学版, 2011, 38(1):7-14. Google Scholar
[22]	杨作升, 赵晓辉, 乔淑卿, 等.长江和黄河入海沉积物不同粒级中长石/石英比值及化学风化程度评价[J]. 中国海洋大学学报:自然科学版, 2008, 38(2):244-250. Google Scholar
[23]	王策, 梁新权, 童传新, 等.莺歌海盆地东北部邻区7条主要入海河流重砂矿物特征及其地质意义[J]. 沉积学报, 2014, 32(2):228-237. Google Scholar
[24]	付玲, 关平, 赵为永, 等.柴达木盆地古近系路乐河组重矿物特征与物源分析[J]. 岩石学报, 2013, 29(8):2867-2875. Google Scholar
[25]	陈心怡, 黄奇瑜, 邵磊. 福建闽江和九龙江现代沉积物重矿物特征及其物源意义[J]. 古地理学报, 2018, 20(4):637-650. Google Scholar
[26]	王利波, 李军, 赵京涛, 等.辽东湾周边河流沉积物碎屑矿物组成及其物源意义[J]. 沉积学报, 2013, 31(4):663-671. Google Scholar
[27]	刘光鼎.中国海区及邻域地质地球物理系列图[M]. 北京:科学出版社, 1996:5-34. Google Scholar
[28]	许东禹, 刘锡清, 张训华, 等.中国近海地质[M]. 北京:地质出版社, 1997:6-13. Google Scholar
[29]	蒋仁, 曾剑威, 刘凯, 等. 江苏洋口港地区埋藏古潮成砂脊年代学特征及古环境意义[J]. 华东地质, 2019, 40(1):11-18. Google Scholar
[30]	TELEKI P G, DOBSON M R, MOORE J R, et al. Marine Minerals:Advances in Research and Resource Assessment[M]. Dordrecht:Reidel Publishing Company, 1987:39-56. Google Scholar
[31]	顾佳, 闫玉茹, 平利姣.南通近海潮滩表层沉积物重金属含量特征与生态风险评价[J]. 华东地质, 2017, 38(2):155-160. Google Scholar