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琼东北八所组ESR年龄及其构造意义

夏蒙蒙 王超群 胡道功 赵希涛 贾丽云 吴环环 吕同艳

夏蒙蒙, 王超群, 胡道功, 等, 2019. 琼东北八所组ESR年龄及其构造意义. 地质力学学报, 25 (2): 257-266. DOI: 10.12090/j.issn.1006-6616.2019.25.02.025
引用本文: 夏蒙蒙, 王超群, 胡道功, 等, 2019. 琼东北八所组ESR年龄及其构造意义. 地质力学学报, 25 (2): 257-266. DOI: 10.12090/j.issn.1006-6616.2019.25.02.025
XIA Mengmeng, WANG Chaoqun, HU Daogong, et al., 2019. ESR DATING OF THE BASUO FORMATION IN THE NORTHEASTERN HAINAN ISLAND AND ITS TECTONIC SIGNIFICANCE. Journal of Geomechanics, 25 (2): 257-266. DOI: 10.12090/j.issn.1006-6616.2019.25.02.025
Citation: XIA Mengmeng, WANG Chaoqun, HU Daogong, et al., 2019. ESR DATING OF THE BASUO FORMATION IN THE NORTHEASTERN HAINAN ISLAND AND ITS TECTONIC SIGNIFICANCE. Journal of Geomechanics, 25 (2): 257-266. DOI: 10.12090/j.issn.1006-6616.2019.25.02.025

琼东北八所组ESR年龄及其构造意义

doi: 10.12090/j.issn.1006-6616.2019.25.02.025
基金项目: 

中国地质调查局项目 DD20190306

中国地质调查局项目 DD20160269

详细信息
    作者简介:

    夏蒙蒙(1992-), 女, 在读硕士, 从事新构造与活动构造研究。E-mail:2831419942@qq.com

    通讯作者:

    胡道功(1963-), 男, 研究员, 从事新构造与活动构造研究。E-mail:hudg@263.net

  • 中图分类号: P534.63

ESR DATING OF THE BASUO FORMATION IN THE NORTHEASTERN HAINAN ISLAND AND ITS TECTONIC SIGNIFICANCE

  • 摘要: 八所组是琼东北晚第四纪一个重要地层单位,同时也是河流Ⅱ级阶地(T2)的主要沉积地层,其形成年代对该区域晚第四纪以来的古环境演化及地壳运动的研究有着重要意义。为了限定其形成时代,文章采取ESR的方法,对广泛分布于琼东北珠溪河及古三江河一带的八所组地层进行了系统的测年。结果表明:该套地层形成于晚更新世中晚期(64.36 ka~18.40 ka BP);沉积时代对应末次冰期MIS4~MIS2阶段;河流的下切与T2阶地的形成,一定程度上反映了该时期琼东北海平面的频繁波动及地壳的间歇性抬升;此外,分布于现代海岸风沙强烈作用地带的老红砂与八所组属同期异相的风成堆积,应与八所组地层加以区分。

     

  • 图  1  琼北地区地质简图及已发表年龄分布图

    Figure  1.  Simplified geological map of northern Hainan Island and the distribution of the published ESR dating of the Basuo Formation

    图  2  八所组沉积地层及采样位置

    Figure  2.  Sedimentary strata and sampling locations of the Basuo Fermation

    图  3  八所组样品ESR年龄分布图

    Figure  3.  The location of ESR dating of the samples from the Basuo Formation

    图  4  代表性样品电子自旋共振(ESR)谱图

    a-样品B007-1电子自旋共振图谱;b-样品QZ25-6电子自旋共振图谱

    Figure  4.  Typical ESR resonance spectra of quartz extracted from the samples

    图  5  琼东北地层横切剖面图

    Figure  5.  Cross stratigraphic section in the northeastern Hainan Island

    表  1  八所组ESR测年样品位置表

    Table  1.   ESR dating locations of samples from the Basuo Formation

    样品编号 采样
    地点
    样品经纬度 海拔
    /m
    采样
    层位
    岩性及取样
    深度/m
    剖面厚度
    /m
    地貌部位
    B170-1(地表样品) 文堆村 19°58′9.3″N, 110°46′4.09″E 5 顶部 灰黄色粉细砂 0.5 T2(贝坡河)
    B247-1(地表样品) 正纪村 20°03′08.0″N, 110°38′27.6″E 8 顶部 灰黄色中细砂 0.9 T2(珠溪河)
    B251-1(地表样品) 南坑村 20°01′27.4″N, 110°42′05.3″E 8 顶部 黄褐色中粗砂 0.4 T2(潮滩河)
    B134-1(地表样品) 桃丛村 19°52′37.65″N, 110°46′27.2″E 20 中部 灰黄色中细砂 0.75 T2(贝坡河)
    B515-1(地表样品) 老村 19°51′13.21″N, 110°42′15.5″E 21 顶部 灰白色中细砂 0.3 T2(贝坡河)
    B207-1(地表样品) 后坡村 19°59′28.4″N, 110°39′33.4″E 8 顶部 黄褐色中细砂 0.6 T2(东寨河)
    B007-1(地表样品) 双堆坡 19°54′16.17″N, 110°42′11.5″E 17 底部 灰白色中细砂 0.5 T2(贝坡河)
    B160-1(地表样品) 坡坞园 20°2′10.05″N, 110°45′19.3″E 13 顶部 黄褐色粉细砂 0.45 T2(贝坡河)
    B154-1(地表样品) 茂山坡 19°54′42.58″N, 110°43′39.8″E 20 中部 灰黄色粉细砂 0.4 T2(贝坡河)
    B151-1(地表样品) 上良安 19°56′2.39″N, 110°42′19.9″E 19 顶部 灰黄色粉细砂 0.5 T2(贝坡河)
    B168-1(地表样品) 白茅村 19°58′44.3″N, 110°44′24.3″E 8 底部 灰白色粉细砂 0.5 T2(贝坡河)
    QZ33-4(钻孔样品) 桥坡村 20°02′23.6″N, 110°42′07.3″E 3 顶部 黄褐色中细砂 1.5 T2(珠溪河)
    QZ23-5(钻孔样品) 后坡郭 19°58′42.6″N, 110°39′14.7″E 3 中部 灰白色中细砂 13 T2(东寨河)
    QZ24-8(钻孔样品) 昌沟洋 19°57′34.1″N, 110°39′58.0″E 3 顶部 黄褐色中细砂 8 T2(东寨河)
    QZ32-3(钻孔样品) 桥坡村 20°02′24.5″N, 110°42′07.3″E 4 顶部 黄褐色中细砂 2 T2(珠溪河)
    QZ25-6(钻孔样品) 新龙坡 19°57′23.9″N, 110°39′58.1″E 2 底部 灰白色中细砂 5 T2(东寨河)
    下载: 导出CSV

    表  2  八所组ESR测年结果数据表

    Table  2.   ESR dating results of samples from the Basuo Formation

    样品编号 样品埋深/
    m
    古剂量/
    Gy
    年吸收量/
    mGy
    铀含量/
    (ug/g)
    钍含量/
    (ug/g)
    钾含量/
    (ug/g)
    年龄/
    ka
    地表样品
    B170-1 0.3 31.98 1.580 1.02±0.10 3.13±0.30 0.59±0.05 20.24±2.00
    B247-1 0.5 64.45 2.870 2.79±0.28 8.65±0.85 0.61±0.05 22.45±2.20
    B251-1 0.2 71.45 2.700 2.56±0.25 7.92±0.75 0.60±0.05 26.53±2.60
    B134-1 0.4 83.41 2.654 2.56±0.25 7.57±0.70 0.55±0.05 31.40±3.10
    B515-1 0.5 75.95 2.360 2.10±0.02 6.53±0.60 0.58±0.05 32.18±3.20
    B207-1 0.3 61.32 1.660 1.19±0.10 3.59±0.35 0.55±0.05 36.94±3.50
    B007-1 0.3 63.13 1.686 1.30±0.13 3.01±0.30 0.48±0.04 37.40±3.50
    B160-1 0.2 128.24 3.000 2.93±0.25 9.09±0.90 0.64±0.05 42.75±4.20
    B154-1 0.2 156.68 3.110 3.09±0.30 9.29±0.90 0.64±0.55 50.38±5.00
    B151-1 0.4 176.19 2.950 2.79±0.25 8.78±0.65 0.70±0.05 59.73±5.90
    B168-1 0.4 106.84 1.660 1.13±0.10 3.55±0.30 0.59±0.05 64.36±6.40
    钻孔样品
    QZ33-4 1.3 119.09 6.470 1.64±0.15 15.73±1.50 2.77±1.50 18.40±1.80
    QZ23-5 3.9 121.27 6.230 5.25±0.50 15.81±1.50 2.41±0.20 19.46±1.80
    QZ24-8 6.1 69.23 2.970 1.12±0.12 3.32±0.30 2.11±0.20 23.31±2.30
    QZ32-3 1.3 114.61 4.770 3.62±0.35 10.46±1.00 2.33±0.23 24.03±2.40
    QZ25-6 4.9 256.82 4.240 2.96±0.28 9.56±0.90 1.99±0.15 60.57±6.00
    下载: 导出CSV
  • [1] 莫位任, 朱耀河, 袁勤敏, 等.海南文昌地区第四系沉积物特征及其地质意义[J].华南地质与矿产, 2015, 31(1):1~10. doi: 10.3969/j.issn.1007-3701.2015.01.001

    MO Weiren, ZHU Yaohe, YUAN Qinmin, et al. The characteristics and geological significance of quaternary sediments from Wenchang area of Hainan province[J]. Geology and Mineral Resources of South China, 2015, 31(1):1~10. (in Chinese with English abstract doi: 10.3969/j.issn.1007-3701.2015.01.001
    [2] 李冬环, 吴正.浙江普陀山岛老红砂的成因与环境[J].地理科学, 2005, 25(6):716~719. doi: 10.3969/j.issn.1000-0690.2005.06.011

    LI Donghuan, WU Zheng. Origin and circumstance of old red sand sediment on Putuo Island[J]. Scientia Geographica Sinica, 2005, 25(6):716~719. (in Chinese with English abstract doi: 10.3969/j.issn.1000-0690.2005.06.011
    [3] 汪啸风, 马大铨, 蒋大海.海南岛地质(一):地层古生物[M].北京:地质出版社, 1992, 131~192.

    WANG Xiaofeng, MA Daquan, JIANG Dahai. Geology and stragraphic paleontology of Hainan Island[M]. Beijing:Geological Publishing House, 1992, 131~192. (in Chinese)
    [4] 吴正, 黄山, 金志敏, 等.华南沿海老红砂的成因与红化作用[J].地理学报, 1994, 49(4):298~306. doi: 10.3321/j.issn:0375-5444.1994.04.003

    WU Zheng, HUANG Shan, JIN Zhimin, et al. Research on the formation and laterization of the "old red sandy sediment" along the coast of South China[J]. Acta Geographica Sinica, 1994, 49(4):298~306. (in Chinese with English abstract doi: 10.3321/j.issn:0375-5444.1994.04.003
    [5] 海南省地质调查院. 1/5万昌洒市幅、文昌县幅、清澜港幅、铜鼓咀幅区域地质调查报告[R].海口: 海南省地质调查院, 2005.

    The Geological Survey Institute of Hainan. Regional geological map and survey of Changsa county/Wenchang county/Qinglan/Tongguzui at 1: 50000 in Hainan Province[R]. Haikou: The Geological Survey Institute of Hainan, 2005. (in Chinese)
    [6] 袁宝印.海南岛北部第四纪玄武岩分期问题[A].中国地理学会第一次构造地貌学术讨论会论文选集[C].北京: 科学出社, 1984, 182~187.

    YUAN Baoyin. The issue of basalt stage in the northern part of Hainan Island[A]. The first Geological Symposium Selected Papers of the Chinese Geography Society[C]. Beijing: Science Press, 1984, 1820~187. (in Chinese)
    [7] 刘瑞华, 张仲英, 韩中元.海南岛西部砂地的成因探讨[J].热带地理, 1986, 6(3):256~263.

    LIU Ruihua, ZHANG Zhongying, HAN Zhongyuan. On the origin of sandy land in west part of Hainan Island[J]. Tropical Geography, 1986, 6(3):256~263. (in Chinese with English abstract
    [8] 闫成国, 江娃利.琼北地区北西方向长流-仙沟断裂带晚第四纪活动及与火山活动关系的讨论[J].震灾防御技术, 2007, 2(3):230~242. doi: 10.3969/j.issn.1673-5722.2007.03.002

    YAN Chengguo, JIANG Wali. Relationship between the activity of the Changliu-Xiangou fault zone in late-quaternary and volcanic activity in North Hainan Island[J]. Technology for Earthquake Disaster Prevention, 2007, 2(3):230~242. (in Chinese with English abstract doi: 10.3969/j.issn.1673-5722.2007.03.002
    [9] 丁莹莹, 赵希涛, 胡道功, 等.琼东北晚新生代断裂活动及其对东寨港沉降的控制作用[J].地球学报, 2018, 39(2):155~166. http://d.old.wanfangdata.com.cn/Periodical/dqxb201802004

    DING Yingying, ZHAO Xitao, HU Daogong, et al. Late Cenozoic fault activity in Northeastern Hainan Island and its controlling effect on tectonic subsidence in Dongzhai port[J]. Acta Geoscientica Sinica, 2018, 39(2):155~166. (in Chinese with English abstract http://d.old.wanfangdata.com.cn/Periodical/dqxb201802004
    [10] 张虎男, 赵希涛.雷琼地区新构造运动的特征[J].地质科学, 1984, 19(3):276~287. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198403004.htm

    ZHANG Hunan, ZHAO Xitao. Characteristics of the neotectonic movement in the Hainan Island and Leizhou Peninsula area[J]. Chinese Journal of Geology, 1984, 19(3):276~287. (in Chinese with English abstract http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198403004.htm
    [11] Zhao F, Alves T M, Wu S G, et al. Prolonged post-rift magmatism on highly extended crust of divergent continental margins (Baiyun sag, South China sea)[J]. Earth and Planetary Science Letters, 2016, 445:79~91. doi: 10.1016/j.epsl.2016.04.001
    [12] 海南省地质调查院.海南省1: 25万琼海县幅区域地质图和调查报告[R].海口: 海南省地质调查院, 2004.

    The Geological Survey Institute of Hainan. Regional geo-logical map and survey of Qionghai county at 1: 25 in Hainan Province[R]. Haikou: The Geological Survey Institute of Hainan, 2004. (in Chinese)
    [13] 徐起浩. 1605年琼州大地震陆陷成海和可能的海啸[J].海洋学报, 2007, 29(3):146~156. doi: 10.3321/j.issn:0253-4193.2007.03.020

    XU Qihao. The land sank into the sea and possible tsunami by the great earthquake in Qiongzhou in China in 1605[J]. Acta Oceanologica Sinica, 2007, 29(3):146~156. (in Chinese) doi: 10.3321/j.issn:0253-4193.2007.03.020
    [14] 陈恩民, 黄咏茵. 1605年海南岛琼州大地震及其发震构造的初步探讨[J].地震地质, 1979, 1(4):37~44.

    CHEN Enmin, HUANG Yongyin. Preliminary discussion on the 1605 Qiongzhou earthquake and its seismogenetic structure[J]. Seismology and Geology, 1979, 1(4):37~44. (in Chinese with English abstract
    [15] 徐起浩.琼北东寨港地区的近期下沉[J].海洋科学, 1986, 10(1):24~28.

    XU Qihao. Recent sinking in the Dongzhai Harbour area, Northern Qiongzhou[J]. Marine Sciences, 1986, 10(1):24~28. (in Chinese with English abstract
    [16] 金志敏, 廖秉良, 吴正.华南沿海"老红砂"红化作用研究[J].科学通报, 1994, 39(12):1122~1124. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199412018.htm

    JIN Zhimin, LIAO Bingliang, WU Zheng. Research on the laterization of the "Old Red Sediment" along the coast of South China[J]. Chinese Science Bulletin, 1994, 39(12):1122~1124. (in Chinese) http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199412018.htm
    [17] Gardner R, Pye K. Nature, origin and palaeoenvironmental significance of red coastal and desert dune sands[J]. Progress in Physical Geography:Earth and Environment, 1981, 5(4):514~534. doi: 10.1177/030913338100500402
    [18] 孙宏利.福建平潭岛海岸风沙地貌研究[D].广州: 华南师范大学, 1994.

    SUN Hongli. Research on coastal sandy landforms of Pingtan Island, Fujian Province[D]. Guangzhou: South China Normal University, 1994. (in Chinese)
    [19] 许峰宇, 王为.海南文昌涣文村老红砂剖面的磁化率测量及意义[J].中国沙漠, 1996, 16(4):364~367. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGSS604.007.htm

    XU Fengyu, WANG Wei. Measurement and Its significance of magnetic susceptibility of Huanwen "Old Red Sandy Sediment" section in Wenchang county of Hainan Island[J]. Journal of Desert Research, 1996, 16(4):364~367. (in Chinese with English abstract http://www.cnki.com.cn/Article/CJFDTOTAL-ZGSS604.007.htm
    [20] 徐起浩.海南岛东寨港成因新说[J].地球, 1988, (4):10~11. http://epub.cnki.net/grid2008/detail.aspx?filename=DIQU198804010&dbname=CJFN1988

    XU Qihao. The new understanding of the formation of Dongzhai Port[J]. The Earth, 1988, (4):10~11. (in Chinese) http://epub.cnki.net/grid2008/detail.aspx?filename=DIQU198804010&dbname=CJFN1988
    [21] 徐起浩.海南岛北部东寨港的形成、变迁与1605年琼州大地震[J].地震地质, 1986, 8(3):92~96. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ198603012.htm

    XU Qihao. Formation and migration of Dongzhai port in the northern Hainan Island and the major Qiongzhou earthquake of 1605[J]. Seismology and Geology, 1986, 8(3):92~96. (in Chinese with English abstract http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ198603012.htm
    [22] 彭承光. 1605年7月13日琼州历史地震陆沉原因[J].地震地质, 1983, 5(3):9~15.

    PENG Chengguang. Cause of the land subsidence associated with the historical Qiongzhou earthquake (13 July 1605)[J]. Seismology and Geology, 1983, 5(3):9~15. (in Chinese with English abstract
    [23] 刘晓佳, 赵立国, 田珺, 等.漠河逆冲推覆构造活动时代的ESR年龄证据[J].地质力学学报, 2014, 20(3):299~303. doi: 10.3969/j.issn.1006-6616.2014.03.009

    LIU Xiaojia, ZHAO Liguo, TIAN Jun, et al. ESR ages evidences of Mohe overthrust structure stage[J]. Journal of Geomechanics, 2014, 20(3):299~303. (in Chinese with English abstract doi: 10.3969/j.issn.1006-6616.2014.03.009
    [24] 戚帮申, 胡道功, 王进寿, 等.中祁连木里盆地古近系ESR年龄及地质意义[J].地质力学学报, 2013, 19(4):392~402. doi: 10.3969/j.issn.1006-6616.2013.04.005

    QI Bangshen, Hu Daogong, WANG Jinshou, et al. ESR Dating of the Palaeogene in Muli basin in the middle of Qilian Mountains and its geological significance[J]. Journal of Geomechanics, 2013, 19(4):392~402. (in Chinese with English abstract doi: 10.3969/j.issn.1006-6616.2013.04.005
    [25] 梁兴中, 高钧成.断裂成矿年龄的α石英ESR研究[J].矿物岩石, 1999, 19(2):69~71. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900416170

    LIANG Xingzhong, GAO Juncheng. Study on the α-quartz dating of fault-related ore mineralization[J]. Journal of Mineralogy and Petrology, 1999, 19(2):69~71. (in Chinese with English abstract http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900416170
    [26] 韩建恩, 郭长宝, 吴瑞安, 等.川西岷江松潘段第四纪与新构造运动特征分析[J].地质力学学报, 2017, 23(6):864~881. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20170608&journal_id=dzlxxb

    HAN Jian'en, GUO Changbao, WU Ruian, et al. Characteristics analysis of quaternary and neotectonic movements from Songpan section, Minjiang upper reaches, Western Sichuan[J]. Journal of Geomechanics, 2017, 23(6):864~881. (in Chinese with English abstract http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20170608&journal_id=dzlxxb
    [27] 樊祺诚, 孙建中.琼北第四纪玄武岩的岩石学和地球化学[J].科学通报, 1987, 32(4):287~291. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB198704013.htm

    FAN Qicheng, SUN Jianzhong. Petrology and geochemistry of quaternary basalt in North Hainan Island[J]. Chinese Science Bulletin, 1988, 33(11):925~929. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB198704013.htm
    [28] 曾兰华, 李森, 李保生, 等.海南岛西部八所组上部砂质沉积物的成因及其环境意义[J].地质论评, 2007, 53(6):783~790. doi: 10.3321/j.issn:0371-5736.2007.06.012

    ZENG Lanhua, LI Sen, Li Baosheng, et al. The genesis and environmental significance of the sandy sediments of the Upper Basuo formation in western Hainan Island[J]. Geological Review, 2007, 53(6):783~790. (in Chinese with English abstract). doi: 10.3321/j.issn:0371-5736.2007.06.012
    [29] 张仲英, 刘瑞华, 韩中元.海南岛沿海的第四纪地层[J].热带地理, 1987, 7(1):54~64. http://www.cnki.com.cn/Article/CJFDTOTAL-RDDD198701006.htm

    ZHNAG Zhongying, LIU Ruihua, HAN Zhongyuan. The quaternary stratigraphy along the coastal area of Hainan Island[J]. Tropical Geography, 1987, 7(1):54~64. (in Chinese with English abstract http://www.cnki.com.cn/Article/CJFDTOTAL-RDDD198701006.htm
    [30] Schumm S A. River response to baselevel change:implications for sequence stratigraphy[J]. The Journal of Geology, 1993, 101(2):279~294. doi: 10.1086/648221
    [31] 周青硕, 张绪教, 叶培盛, 等.河套地区全新世黄河古河道的分布及期次划分[J].地质力学学报, 2017, 23(3):339~347. doi: 10.3969/j.issn.1006-6616.2017.03.002

    ZHOU Qingshuo, ZHANG Xujiao, YE Peisheng, et al. The distribution and period division of Holocene Palaeo channels of the Yellow River in Hetao area[J]. Journal of Geomechanics, 2017, 23(3):339~347. (in Chinese with English abstract doi: 10.3969/j.issn.1006-6616.2017.03.002
    [32] Clark P U, Dyke A S, Shakun J D, et al. The last glacial maximum[J]. Science, 2009, 325(5941):710~714. doi: 10.1126/science.1172873
    [33] 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.

    XU Dongyu, LIU Xiqing, ZHANG Xunhua, et al. China offshore geology[M]. Beijing:Geological Publishing House, 1997. (in Chinese).
    [34] 吴正, 冯文科, 廖秉良, 等.晚更新世末期南海北部陆架的古地理探讨[J].地理学报, 1993, 48(6):491~496. doi: 10.3321/j.issn:0375-5444.1993.06.002

    WU Zheng, FENG Wenke, LIAO Bingliang, et al. Papaeogeographic study in the continental shelf of the northern South China Sea during the Last Stage of the late Pleistocene[J]. Acta Geographica Sinica, 1993, 48(6):491~496. (in Chinese with English abstract doi: 10.3321/j.issn:0375-5444.1993.06.002
    [35] 贺子丁, 刘志飞, 李建如, 等.南海西部54万年以来元素地球化学记录及其反映的古环境演变[J].地球科学进展, 2012, 27(3):327~336. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz201203010

    HE Ziding, LIU Zhifei, LI Jianru, et al. Elemental geochemical records in the western South China Sea since 540 ka and their paleoenvironmental implications[J]. Advances in Earth Science, 2012, 27(3):327~336. (in Chinese with English abstract http://d.old.wanfangdata.com.cn/Periodical/dqkxjz201203010
    [36] 赵松龄, 于洪军, 刘敬圃.晚更新世末期陆架沙漠化环境演化模式的探讨[J].中国科学(D辑), 1996, 26(2):142~146. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600264805

    ZHAO Songling, YU Hongjun, LIU Jingpu. Origin, development and evolutionary model of shelf desertization environment in late stage of Upper Pleistocene[J]. Science in China Series D:Earth Sciences, 1997, 40(2):207~214. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600264805
    [37] 廖肖霞, 李森, 王贵勇, 等. 38ka以来海南岛东海岸风成沙的粒度特征及其反映的沉积环境演变过程[J].中国沙漠, 2009, 29(6):1086~1092. http://d.old.wanfangdata.com.cn/Periodical/zgsm200906013

    LIAO Xiaoxia, LI Sen, WANG Guiyong, et al. Grain-size features of Aeolian sands on eastern coast of Hainan Island and the reflected sedimentary environment since 38 ka BP[J]. Journal of Desert Research, 2009, 29(6):1086~1092. (in Chinese with English abstract http://d.old.wanfangdata.com.cn/Periodical/zgsm200906013
    [38] 李森, 廖肖霞, 王贵勇.近40ka来海南岛海岸沙地气候与环境演变[J].地理研究, 2009, 28(5):1235~1242. doi: 10.3321/j.issn:1000-0585.2009.05.010

    LI Sen, LIAO Xiaoxia, WANG Guiyong, et al. Climatic and environmental changes in the coastal sandy land of Hainan Island in recent 40 ka[J]. Geographical Research, 2009, 28(5):1235~1242. (in Chinese with English abstract doi: 10.3321/j.issn:1000-0585.2009.05.010
    [39] 毕福志, 韩慕康, 赵叔松, 等.海南岛东寨港罗豆农场的海月沉积层及其海岸升降特征[J].海洋通报, 1988, 7(3):35~40.

    BI Fuzhi, HAN Mukang, ZHAO Shusong, et al. Sea-moon sedimentary layer and its coastal lifting characteristics of Luodou Farm in Dongzhai Port, Hainan Island[J]. Marine Science Bulletin, 1988, 7(3):35~40. (in Chinese).
    [40] 李建生, 杨基广.海南岛罗豆地区的贝壳堤[J].海洋科学, 1991, (6):73. http://www.cnki.com.cn/Article/CJFDTOTAL-HYKX199106032.htm

    LI Jiansheng, YANG Jiguang. Shell embankment in the Luodou area of Hainan Island[J]. Marine Sciences, 1991, (6):73. (in Chinese). http://www.cnki.com.cn/Article/CJFDTOTAL-HYKX199106032.htm
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  • 收稿日期:  2018-05-09
  • 修回日期:  2018-09-10
  • 刊出日期:  2019-04-28

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