南海及其周缘地区全新世海平面遗迹的构造含义

孙桂华; 邱燕; 朱本铎

南海及其周缘地区全新世海平面遗迹的构造含义

国土资源部广州海洋地质调查局, 广东广州 510760

基金项目: 国土资源大调查项目资助(1212010611302)

计量
- 文章访问数: 1259
- HTML全文浏览量: 12
- PDF下载量: 1418
- 被引次数: 0
出版历程
- 收稿日期: 2008-12-22
- 修回日期: 2009-06-06

The tectonic implications of Holocene sea-level relics in the South China Sea and adjacent areas

Guangzhou Marine Geological Survey Bureau, Ministry of Land and Natural Resources, Guangzhou 510760, China

摘要

摘要: 通过对海南岛海岸带野外考察,在文昌市铜鼓岭石头公园观察到高程为30m的海平面遗迹,在东方市黄流镇观察到高程为25~35m的海平面遗迹,在三亚市鹿回头观察到高程为2.5m的海平面遗迹。综合研究前人在该区关于海平面变化的研究成果,得出如下几点初步认识:(1)南海及其周缘地区中全新世以来海平面呈下降趋势,海平面最高位置出现在7000a左右、高于现代海平面3m左右的位置;(2)南海中全新世以来海平面遗迹所揭示的古海平面高程的差异性是古海平面本身持续下降和该区地壳差异性垂直运动共同作用的结果;(3)南海及其周缘地区中全新世期间中央海盆及其西缘的珠江口、红河、湄公河和昭披耶河4个河流三角洲地区为构造沉降区,而南海周缘的台湾岛、雷州半岛、印支半岛、南马来半岛、爪哇岛和苏拉威西岛6个地区为构造抬升区,抬升幅度最大的地方在台湾岛。
- 海平面遗迹 /
- 中全新世 /
- 地壳差异性垂直运动 /
- 南海及其周缘地区
Abstract: Three sea level relics were introduced based on the investigation of the Hainan Island coastal zone: the sea level relic of the Shitou Park, Tongguling of Wenchang City with 30 m height above present-day sea level, the sea level relic of Huangliu Town of Dongfang City with 25～35 m height above present-day sea level, and the sea level relic of Luhuitou of Sanya City with 2.5 m height above present-day sea level. The following several conclusions are got based on the synthetical research of other scientist's study results about the change of sea level. First, the sea level of the South China Sea and adjacent areas has had falling tendency since mid-Holocene, and the highest height is 3 m above present-day sea level with the emergence geolo gical age of 7 ka. Second, the height's otherness of paleo sea-level of the South China Sea and adjacent areas since mid-Holocene that has been displayed by sea level relics is the conjunct result of paleo sea-level continuance descend and otherness vertical movement of crust. Finally, the central ocean basin, and the deltas of Zhujiang River, Red River, Mekong River and Zhaopiye River were structural subsidence areas, but Taiwan Island, the Leizhou Peninsula, the Indochina Peninsula, the South Malaya Peninsula, Java Island and Sulawesi Island were structural uplifted areas in the South China Sea and adjacent areas during mid-Holocene, and the biggest amplitude of structural uplift was located in Taiwan Island.
- sea level relics /
- mid-Holocene /
- otherness vertical movement of crust /
- South China Sea and adjacent areas

HTML全文

参考文献(54)

丁荣荣,左军成,杜凌,等.南海海平面变化及其比容高度和风场间的关系[J].中国海洋大学学报,2007,37(增刊Ⅱ):23-30.

荣增瑞,刘玉光,陈满春,等.全球和南海海平面变化及其与厄尔尼诺的关系[J].海洋通报,2008,27(1):1-8.

黄镇国,张伟强.南海现代海平面变化研究的进展[J].台湾海峡.2004,23(4):530-535.

乔新,陈戈.基于11年高度计数据的中国海海平面变化初步研究[J].海洋科学,2008,32(1):60－64.

黄德银,施祺,张叶春.海南岛鹿回头珊瑚礁与全新世高海平面[J].海洋地质与第四纪地质,2005.25(4):1-7.

王国忠.全球海平面变化与中国珊瑚礁[J].古地理学报.2005,7(4):483-492.

聂宝符,陈特固,梁美桃,等.南沙群岛及其邻近礁区造礁珊瑚与环境变化的关系[M].北京:科学出版社,1997:62-63.

赵希涛,杨达源.全球海面变化[M].北京:科学出版社,1992:8-27.

赵希涛,张景文,李桂英.海南岛南岸全新世珊瑚礁发育口].地质科学,1983(2):150-159

陈俊仁,陈欣树,赵希涛,等.全新世海南省鹿回头海平面变化之研究[G]//南海地质研究(三).广州:广东省科学技术出版社,1991:77-86.

KOROTKY A M,RAZJIGAEVA N G,GANZEY L A,et al.Late Pleistocene-Holocene coastal development of islands off Vietnam[J].Journal of Southeast Asian Earth Sciences,1995,11(4):301-308.

CHEN Yue-gau,LIU Tsung-kwei.Sea level changes in the last several thousand years,Penghu Islands,Taiwan Strait[J].Quaternary Research,1995,45:254-262.

聂宝符,陈特固,梁美桃,等.雷州半岛珊瑚礁与全新世高海面[J].科学通报,1997.42(5):511-514.

余克服,钟晋梁.赵建新,等.雷州半岛珊瑚礁生物地貌带与全新世多期相对高海平面[J].海洋地质与第四纪地质,2002,22(2):27-33.

杨建明,郑晓云.福建沿岸6000年来的海平面波动[J].海洋地质与第四纪地质,1990,10(4):67-74.

方国祥,李平日,黄光庆.闽南粤东全新世海平面变化[J].第四纪研究,1992,12(3):233-239.

TJIA H D.Sea-level changes in the tectonically stable MalayThai Peninsula[J].Quaternary International,1996,31:95-101.

GEYH M A,KUDRASS H R.Sea level changes during the late Pleistocene and Holocene in the Strait of Malacca[J].Nature,1979,278:441-443.

YIM W W S,HUANG G.Middle Holocene higher sea level in dicators from the South China coast[J].Marine Geology,2002,183(324):225-230.

陈俊仁,李学杰.珠海钻孔剖面沉积特征与海平面变化[G]//南海地质研究(八).武汉:中国地质大学出版社.1996:67-96.

BERDIN R D,S1RINFAN F P,YASUO Maed.Holocene sea level high stand and its implications for the vertical stability of Panglao Is-land,southwest Bohol,Philippines[J].Quaternary International,2004,115-116:27-37.

张虎南.陈伟光,黄坤容,等.华南沿海新构造运动与地质环境[M].北京:地震出版杜,1990:237.

YU Ke-fu.ZHAO Jian-xin,LIU Tung-sheng,et al.High frequency winter cooling and red coral mortality during the Holocene climatic optimum[J].Earth and Planetary Science Letters,2004,224:143-155.

聂宝符.五千年来南海海平面变化的研究[J].第四纪研究,1996,16(1):80-87.

薛春汀.对我国沿海全新世海面变化研究的讨论[J].海洋学报,2002,24(4):58-67.

ZONG Yong-qiang.Mid-Holocene sea level high stands along the southeast coast of China[J].Quaternary International,2004,117:55-67.

黄镇国,张伟强.南海地区全新世高海平面遗迹高程的区域差异问题[J].台湾海峡,2005,24(2):228-235.

SMITHERS S G,WOODROFFE C D.Microatolls as sea-level indicators on a mid-ocean atoll[J].Marine Geology,2000,168:61-78.

COLLINS L B,ZHAO Jian-xin,HEATHER Freeman.A high-precision record of mid-late Holocene sea-level events from emergent coral Davements in the Hoytman Abrolhos Islands,southwest Australia[J].Quaternary International,2006,145-146:78-85.

赵希涛.中国海岸演变研究[M].福州:福建省科学技术出版社.1984:20-35.

黄镇国,张伟强,许世远,等.中国日本全新世环境演变对比研究[M].广州:广东省科学技术出版社,2002:750-754.

李平日,黄镇国,宗永强,等.韩江三角洲[M].北京:海洋出版社,1987:88-114.

黄镇国,李平日,张仲英.等.珠江三角洲形成发育演变[M].广州:科学普及出版社,1982:150-176.

莫永杰,李平日,方国祥,等.海平面上升对广西沿海的影响与对策[M].北京;科学出版社,1996:66-78.

刘昭蜀,赵焕庭,范时清,等.南海地质[M].北京:科学出版社,2002,204——230:494-498.

WANG H.Isotasy and Holocene high sea levels in East and Southeast Asia[J].Journal of Southeast Asian Earth Sciences,1992,7(1):17-21.

SOMBOON R P.Paleontological study of the recent marine sediments in the lower central plain,Thailand[J].Journal of Southeast Asi-an Earth Sciences,1988,2(3-4):201-210.

太田阳子.日本的海成阶地及其在环太平洋地区海平面变化和地壳运动中的地位[J].科学,1977,5:281-292.

TJIA H D,SHOJi F,KUNIHIKO K,et al.Radicarbon dates of elevated shorelines,Indonesia and Malaysia,Part 1[J].Quaternary Research.1992,2:187-195

KHOO T T.Geomorphological evolution of the Merbok estuary area and its impact[J].Journal of Southeast Asian Earth Sciences,1996,13(3-5):347-371.

SIN Sinsakul.Late Quaternary geology of the lower central plain,Thailand[J].Journal of Asian Earth Sciences,2000,18(4):415-426.

WILFORD G E.The effects of Late Tertiary and Quatermary tectonic movement on the geomorphological evolution of Brunei and adja-cent parts of Sarawak[J].The Journal of Tropical Geography,1 976,24:50-56.

RIMBAMAN I.The role of sea level changes on the coastal environment of northern West Java[J].Journal of Southeast Asian Earth Sciences.1992,7(1):71-77.

YONEKURA N.Late Quaternary vertical cruat movements in and around the Pacific as deduced from former shoreline data[J].Geody-namics.1983,11:41-50.

黄镇国,李平日,张仲英,等.深圳地貌[M].广州:广东省科学技术出版社,1983:81-136.

MATHERS S.Holocene sedimentary architecture of the Red River Delta,Vietnam[J].Journal of Coastal Research,1999,15(2):314-325.

时小军,余克服,陈特固.南海周边中全新世以来的海平面变化研究进展[J].海洋地质与第四纪地质,2007,27(5):121-132.

王绍武,龚道益.全新世几个特征时期的中国气温[J].自然科学进展,2000,10(4):325-332.

李学杰,韩建修,唐荣革,等.南海北部全新世以来的古气候演变[G].南海地质研究(九).武汉t中国地质大学出版社,1999:86-104.

BAKER R G V,DAVIS A M,ATICHISON J C,et a1.Comment on"Mid-Holocene higher sea level indicators from the south China coast"by YIM W W S and HUANG G[Mar.Geol.2002,182:225-230]:a regional perspective[J].Marine Geology,2003-196:91-98.

ANGULO R J,GIANNINI P C F.KENITIRO Suguio.et al.Relative sea-level changes in the last 5 500 years in southern Brazil(Lagu-na Imbituba region,Santa Catarina State)based on vermetid14C ages[J].Marine Geology,1999,159(124):323-339.

RAMSAY P J.9 000 years of sea-level change along the southern African coastline[J].Quaternary International,1996,31:71-75.

BANJEREE P K.Holocene and Late Pleistocene relative sea level fluctuations along the east coast of India[J].Marine Geology,2000,167:243-260.

SEARLE D J,WOODS D P.Detailed documentation of a Holoeene sea level record in the Perth Region,southern Western Australia[J].Quaternary Research.1 986,26:299-308.

施引文献

资源附件(0)

访问统计