DISTRIBUTION OF HEAVY MINERAL ASSEMBLAGES IN SUBSURFACE SEDIMENTS OF DALIAN BAY AND THEIR IMPLICATIONS FOR PROVENANCE AND ENVIRONMENT
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摘要: 对大连湾近海表层沉积物进行了重矿物的分离和鉴定,探讨该区沉积物中重矿物来源,并对沉积环境及其主控因素进行了分析。研究区沉积物中普遍出现的碎屑重矿物共有29种,其中普通角闪石含量最高,绿帘石和钛铁矿次之。重矿物特征指数及不稳定矿物/稳定矿物比值被用来协助划分矿物组合区,结合重矿物分布特征,研究区可划分为3个矿物组合区,对应3个沉积环境区。近岸浅水区,物质来源单一,动力分选是控制重矿物分布的首要因素,重矿物主要来源于辽东半岛的沿岸冲刷;中部台地及二级岸坡之上,属于相对静水环境区,重矿物分布的主控因素是长途搬运过程中的分选作用,主要是研究区东部海域物质经过较远的距离搬运而来;南部深水区,重矿物分布受到物源、搬运距离以及水动力条件等多重因素的影响,而且源区含有较多稳定矿物,可能与周边海域较强潮流带动下沉积物的再悬浮有关。Abstract: The heavy mineral assemblages and their distribution pattern of the subsurface sediments of the Dalian Bay were preliminarily discussed in this paper in connection with their sources and depositional environments as well as dominant factors. A total of 29 species of heavy mineral were discovered in the study area, dominated by hornblende and followed by epidote and ilmenite. Using heavy mineral characteristic indexes (ATi, GZi, ZTR and UM/SM), and the ratio of stable and unstable mineral as means, we divided the study area into 3 subregions, corresponding to 3 sedimentary environments. In the subregion of shallow water in the north, where dynamic sorting dominated, sediments were mainly derived from the coastal erosion of the Liaodong Peninsula. In the subregion of Central platform, where hydrodynamics was weak and differentiation dominated the distribution of heavy minerals, sediments were from the east of the study area through a long distance of transportation. In the subregion of deep water in the south, where the distribution of heavy minerals were affected by a multiple factors, including source, differentiation and sedimentary environment, the deposition of sediments was supposed to be related to the sediment resuspension driven by strong tidal current.
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Keywords:
- heavy mineral /
- provenance /
- sedimentary environment /
- the Dalian Bay
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[1] Ehrmann W, Kerstin P. The heavy mineral record in the Pliocene to Quaternary sediments of the CIROS-2 drill core, McMurdo Sound, Antarctica[J]. Sedimentary Geology, 1999,128(3-4):223-244.
[2] Preston J, Adrian H, Maria M R, et al. The Provenance of Triassic Continental Sandstones from the Beryl Field, Northern North Sea:Mineralogical, Geochemical, and Sedimentological Constraints[J]. Journal of Sedimentary Research, 2002, 72(1):18-29.
[3] Diekmann B, Gerhard K. 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.
[4] 金翔龙. 东海海洋地质[M]. 北京:海洋出版社, 1988.[JIN Xianglong. The East China Sea Marine Geology[M]. Beijing:Ocean Press,1988.] [5] Luepke G. Opaque minerals as aids in distinguishing beween source and sorting effects on beach-sand mineralogy in southwestern oregon[J]. Journal of Sedimentary Research, 1980, 50(2):489-495.
[6] Liu J, Saito Y, Wang H, et al. Sedimentary evolution of the Holocene subaqueous clinoform off the Shandong Peninsula in the Yellow Sea[J]. Marine Geology, 2007,236(3-4):165-187.
[7] 缪经榜, 刘兴泉. 北黄海和渤海冬季环流动力学的数值试验[J]. 海洋学报, 1989, 11:15-22.[MIAO Jingbang, LIU Xingquan. The numerical test of winter circulation dynamics in the North Yellow sea and Bohai Sea[J].Acta Oceanologica Sinica, 1989 , 11:15-22.]
[8] Hu D X. Upwelling and sedimentation dynamics[J]. Chinese Journal of Oceanology and Limnology, 1984,1:12-19.
[9] 韩康, 张存智, 张砚峰, 等. 大连湾及附近海域潮流场数值模拟[J]. 海洋通报, 1994, 13:20-25.[HAN Kang, ZHANG Cunzhi, ZHANG Yanfeng, et al. Numerical computation of tidal current field in Dalian bay and neighbouring water area[J].Marine Science Bulletin, 1994 , 13:20-25.]
[10] 温国义, 李广雪, 赵东波, 等. 根据AVHRRSST探讨中国北部海域冬季环流演变[J].海洋环境科学, 2008, 27(增2):19-23.[WEN Guoyi, LI Guangxue, ZHAO Dongbo, et al. Analysis on circulation in northern China Sea in winter from AVHRRSST[J].Marine Environmental Science, 2008, 27 (Suppl.2):19-23.]
[11] 王伟, 李安春, 徐方建, 等. 北黄海表层沉积物粒度分布特征及其沉积环境分析[J]. 海洋与湖沼, 2009, 40(5):525-531. [WANG Wei, LI Anchun, XU Fangjian, et al. Distribution of surface sediments and sedimentary envrionment in the North Yellow Sea[J]. Oceanologia et Limnologia sinica, 2009, 40(5):525-531.]
[12] 徐学仁, 张志忠, 等. 应用分光光度法监测大连湾海水COD[J]. 海洋环境科学, 2004, 23(3):58-60. [XU Xueren, ZHANG Zhizhong, et al. Monitoring of COD in sea water by the spectrometry in Dalian Bay[J]. Marine Environmental Science, 2004, 23(3):58-60.]
[13] 王年斌, 周遵春, 等. 大连湾赤潮异弯藻赤潮的多元分析[J]. 海洋学报, 2006, 28(3):151-156. [WANG Nianbin, ZHOU Zunchun, et al. Analysis on multivariate statistics for Heterosigma akashiwo blooming in Dalian Bay[J]. Acta Oceanologica Sinica, 2006, 28(3):151-156.]
[14] 李艳, 李安春, 万世明, 等. 大连湾近海表层沉积物矿物组合分布特征及其物源环境[J]. 海洋地质与第四纪地质, 2009, 29(4):115-121. [LI Yan, LI Anchun, WAN Shiming, et al. Distribution of mineral assemblages in offshore surface sediments of Dalian Bay in the northwestern North Yellow Sea and their provenance and environmental implication[J]. Marine Geology and Quaternary Geology, 2009,29(4):115-121.]
[15] 刘现明, 徐学仁, 张笑天, 等. 大连湾沉积物中PAHS的初步研究[J]. 环境科学学报, 2001, 21(4):507-509. [LIU Xianming, XU Xueren, ZHANG Xiaotian, et al. A preliminary study on PAHs in the surface sediment samples from Dalian Bay[J]. Acta Scientiae Circumstantiae, 2001, 21(4):507-509.]
[16] 徐茂泉, 许文彬, 孙美琴, 等. 福建兴化湾表层沉积物中重矿物组分及其分布特征[J]. 海洋学报, 2004,26(5):74-82. [XU Maoquan, XU Wenbin, SUN Meiqin, et al. The characteristics of heavy minerals composition and distribution in surface sediment from the Xinghua Bay of Fujian[J]. Acta Oceanologica Sinica, 2004, 26(5):74-82.]
[17] 王琦, 杨作升. 黄海南部表层沉积物中的自生黄铁矿[J]. 海洋与湖沼, 1981, 12(1):25-32. [WANG Qi, YANG Zuosheng. Authigenic pyrite in the surface sediments of the southern Huanghai Sea[J]. Oceanologia et Limnologia Sinica, 1981, 12(1):25-32.]
[18] Giorgetti G, Franco T, Sonia S, et al. Provenance of Pleistocene sediments in the ANDRILL AND-1B drillcore:Clay and heavy mineral data[J]. Global and Planetary Change, 2009, 69(3):94-102.
[19] 王昆山, 石学法, 林振宏. 南黄海和东海北部陆架重矿物组合分区及其来源[J]. 海洋科学进展, 2003, 21(1):31-40. [WANG Kunshan, SHI Xuefa, LIN Zhenhong. Assemblages, provinces and provenances of Heavy Minerals on the shelf of the southern Yellow Sea and northern East China Sea[J]. Advances in Marine Science,2003,21(1):31-40.]
[20] 高建华, 李军, 汪亚军, 等. 鸭绿江河口及近岸海域沉积物中重矿物组成、分布及其沉积动力学意义[J]. 海洋学报, 2009, 31(3):84-94. [GAO Jianhua, LI Jun, WANG Yajun, et al. Heavy mineral distributions and their implications for sediment dynamics in the Yalu Estuary and its adjacent sea area[J]. Acta Oceanologica Sinica, 2009, 31(3):84-94.]
[21] 吕亚男. 山东日照近岸沉积物的重矿物分布与来源[J]. 山东海洋学院学报, 1982, 12(3):43-52. [LV Yanan. Heavy mineral distributions and provenance in coastal sediments of Shandong Rizhao[J]. Periodical of Ocean College of Shandong, 1982, 12(3):43-52.]
[22] Morton A C, Hallsworth C R. Processes controlling the composition of heavy mineral assemblages in sandstones[J]. Sedimentary Geology, 1999,124(1-4):3-29.
[23] Morton A, Hurst A. Correlation of sandstones using heavyminerals:an example from the Statfjord Formation of the Snorre Field, northern North Sea[J]. Geological Society of London, 1995, 89:3-22.
[24] 和钟铧, 刘招君, 郭巍. 柴达木盆地北缘大煤汉剖面重矿物分析及其地质意义[J]. 世界地质, 2001, 20(3):279-284. [HE Zhonghua, LIU Zhaojun, GUO Wei. The heavy mineral analysis and its geological significance of Dameigou section in Northern Caidam Basin[J]. World Geology,2001,20(3):279-284.]
[25] 陈丽蓉. 中国海沉积矿物学[M]. 北京:海洋出版社,2008.[CHEN Lirong. Sediment mineralogy in China Sea[M]. Beijing:Science press, 2008.]
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