关于红海裂谷盆地的构造与沉积输入演化的研究综述

doi:10.3969/j.issn.1000-5641.202092201

摘要/Abstract

摘要：

盆地是一个沉降明显的地区, 在那里可以堆积沉积物. 红海盆地是一个体系的一部分, 其裂谷和胚胎海盆从东非延伸至黎凡特地区, 这是非洲-阿拉伯大陆早渐新世解体形成的. 它是世界上仅有的两个新生裂谷盆地之一, 另一个是伍德拉克盆地, 被认为是研究板块构造现象、沉积形成演化和气候变化的世界最佳自然实验室. 红海是一个年轻的海洋盆地, 从大陆裂谷发育到真正的海洋海底分散. 它包括世界上3.8%的珊瑚礁. 红海盆地的水与世界其他海洋相比是独一无二的, 没有河流流入. 由于缺乏河流输入和永久性河流, 陆源物质仅在暴雨和洪水暴发期间供应. 频繁的沙尘暴(风输送)和钙质生物粉土对海域的塑造很关键. 红海裂谷系统是世界上最大的动态断裂构造体系之一, 它是从最初的裂谷和断裂发展到大陆裂谷的几个阶段, 最后形成大洋板块. 它是监测威尔逊旋回现象的极好场所.

关键词: 红海盆地, 大陆裂谷, 沉积, 威尔逊旋回

Key words: Red Sea basin, continental rift, sedimentary, Wilson Cycle

中图分类号:

P736

ABDUALLAH M. I. Mohamed, 刘堂晏. 关于红海裂谷盆地的构造与沉积输入演化的研究综述[J]. 华东师范大学学报（自然科学版）, 2020, 2020(S1): 74-78.

I. Mohamed ABDUALLAH M., Tangyan LIU. A review about tectonic and sedimentary input evolution of the Red Sea rifting basin[J]. Journal of East China Normal University(Natural Science), 2020, 2020(S1): 74-78.

图/表 4

Fig.1

Fig.2

Table 1

Fig.3

参考文献 20

1	ORMOND R, EDWARDS A. Red Sea fishes [M].[S.l.]: Red Sea, 1987: 251-287.
2	BONATTI E, CIPRIANI A, LUPI L. The Red Sea: Birth of an Ocean [M].[S.l.]: Springer Berlin Heidelberg, 2015: 29-44.
3	AUGUSTIN N, DEVEY C W, DER ZWAN F M, et al. The rifting to spreading transition in the Red Sea. Earth and Planetary Science Letters, 2014, 395, 217- 230.
4	WEGENER A. The Origin of Continents and Oceans (English translation by J. Biram, 1996, of Die Entstehung der Kontinente und Ozeane, revised 4th edition, Braunschweig, Germany Friedr. Vieweg & Sohn) [M]. New York: Dover Publications, Inc., 1929.
5	RASUL N M A, STEWART I C F, NAWAB Z A. Introduction to the Red Sea: Its origin, structure, and environment, in The Red Sea [J].[S.l.]: Springer, 2015: 1-28.
6	BAKER B H, MCCONNELL R B. The Structural Pattern of the Afro-Arabian Rift System in Relation to Plate Tectonics. Philosophical Transactions of the Royal Society A Mathematical Physical & Engineering Sciences, 1970, 267 (1181): 383- 391.
7	GASS I G. The Evolution of Volcanism in the Junction area of the Red Sea, Gulf of Aden and Ethiopian Rifts. Philosophical Transactions of The Royal Society B Biological ences, 1970, 267 (1181): 369- 381.
8	MCKENZIE D, DAVIES D, MOLNAR P, et al. Plate Tectonics of the Red Sea and East Africa. Nature, 1970, 226 (5242): 243- 248.
9	DARRACOTT B W, FAIRHEAD J D, GIRDLER R W. Gravity and magnetic surveys in Northern Tanzania and Southern Kenya. Tectonophysics, 1972, 15 (1-2): 131- 141.
10	BOSWORTH W, HUCHON P, MCCLAY K. The Red Sea and Gulf of Aden Basins. Journal of African Earth ences, 2006, 43 (1-3): 334- 378.
11	HUGHES G W, VAROL O, BEYDOUN Z R. Evidence for Middle Oligocene rifting of the Gulf of Aden and for Late Oligocene rifting of the southern Red Sea. Marine & Petroleum Geology, 1991, 8 (3): 354- 358.
12	WATCHORN F, NICHOLS G J, BOSENCE D W J. Rift-related sedimentation and stratigraphy, southern Yemen (Gulf of Aden)[M]//PURSER B H, BOSENCE D W J. Sedimentation and Tectonics in Rift Basins Red Sea: -Gulf of Aden [J].[S.l.]: Springer, 1998: 165-189.
13	ARBERI F, BORSI S, FERRARA G, et al. Relations between Tectonics and Magmatology in the Northern Danakil Depression (Ethiopia). Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 1970, 293- 311.
14	ZANETTIN B, JUSTIN-VISENTIN E, PICCIRILLO E. Volcanic succession, tectonics and magmatology in central Ethiopia [R]. Soc. cooper. tipogr, 1978.
15	HUGHES G, BEYDOUN Z. The Red Sea—Gulf of Aden: biostratigraphy, lithostratigraphy and palaeoenvironments. Journal of Petroleum Geology, 1992, 15, 135- 156.
16	MATTHEWS D, WILLIAMS C, LAUGHTON A. Mid-ocean ridge in the mouth of the Gulf of Aden. Nature, 1967, 215 (5105): 1052- 1053.
17	SAHOTA G. Geophysical study of the Gulf of Aden continental margins: geodynamic implications for the development of the Afro-Arabian Rift System [D]. Swansea: University College of Swansea, 1991.
18	LEROY S, GENTE P, FOURNIER M, et al. From rifting to spreading in the eastern Gulf of Aden : a geophysical survey of a young oceanic basin from margin to margin. Terra Nova, 2004, 16 (4): 185- 192.
19	BURKE K, DEWEY J F, KIDD W. Precambrian palaeomagnetic results compatible with contemporary operation of the Wilson cycle. Tectonophysics, 1976, 33 (3/4): 287- 299.
20	CONDIE K C. Plate tectonics & crustal evolution [M]. [S.l.]: Elsevier, 2013.

Cruise	Station	Geographical location	Avg. longitude/(E^o)	Avg. latitude/(N^o)	Avg. depth/m
64PE351	13DR	Nereus Deep	37.269	23.210	1672
64PE350	23DR	Hadarba Deep	37.383	22.396	2039
P408-1	26GC	Hariba Deep	38.022	22.040	2008
P408-1	50DR	Hariba Deep	37.898	22.024	2312
P408-1	57DR	Hariba Deep	37.906	22.017	2235
P408-1	19DR	Hariba Deep	37.907	22.012	2226
P408-1	51DR	Hariba Deep	37.927	22.003	2328
P408-1	58DR	Hariba Deep	37.914	22.001	2216
P408-1	18DR	Hariba Deep	37.913	21.996	2219
P408-1	17GC	Hariba Deep	37.911	21.995	2219
P408-1	28GC	Hariba Deep	37.984	21.994	2081
P408-1	29GC	Hariba Deep	38.002	21.937	1962
64PE350	33DR	Atlantis II Deep	38.051	21.403	2072
64PE350	32DR	Discovery Deep	38.030	21.298	1840
64PE350	37DR	Shagara Deep	38.165	21.032	2279
64PE350	41DR	Aswad Deep	38.269	20.869	2264
64PE350	43DR	Erba Deep	38.195	20.737	2331
64PE350	51DR	Port Sudan Deep	38.356	20.192	1916
64PE350	49GC	Port Sudan Deep	38.510	20.037	2701
64PE350	77DR	Suakin Deep	38.753	19.603	2537

[1]	朱宜平, 李小飞, 梁霞. 上海青草沙水库表层沉积物重金属含量水平及其生态风险评价[J]. 华东师范大学学报（自然科学版）, 2021, 2021(2): 54-62.
[2]	黄晶, 郑童童, 王爱华, 栗文静, 王张华. 选择性提取碱土金属元素的方法对比及意义——以宁波平原表层沉积物为例[J]. 华东师范大学学报（自然科学版）, 2021, 2021(2): 73-84.
[3]	ADESINA Rasheed, DADA Olusegun, ASIWAJU-BELLO Yinusa, 贺治国. 尼日利亚海侵泥质海岸粘性沉积物的可蚀性: 初步实验研究[J]. 华东师范大学学报（自然科学版）, 2020, 2020(S1): 120-124.
[4]	余晨笛, 侯立军, 郑艳玲, 刘敏, 尹国宇, 高娟, 刘程, 常永凯. 硝化微生物富集及其种群结构与基因表达分析[J]. 华东师范大学学报(自然科学版), 2019, 2019(3): 164-173.
[5]	许怡雯, 韩静, 何岩, 黄民生. 内源硫影响污染河湖磷营养盐环境行为的研究进展[J]. 华东师范大学学报(自然科学版), 2018, 2018(6): 74-80.
[6]	刘朝; 师育新; 戴雪荣; 席雅娟;. 钱塘江河口区不同河段表层沉积物粒度特征及其对水动力的响应[J]. 华东师范大学学报(自然科学版), 2016, 2016(6): 182-191.
[7]	张密, 文波, 黄凌霞, 杜璟, 邓泓. 氧化还原条件对城市水体沉积物重金属迁移转化的影响[J]. 华东师范大学学报(自然科学版), 2016, 2016(2): 160-.
[8]	李文超, 王文浩, 何岩, 黄民生, 李志洪, 周焜, 朱林林. 黑臭河道沉积物中硫铁行为与氮磷循环的耦合机制[J]. 华东师范大学学报(自然科学版), 2015, 2015(2): 1-8.
[9]	徐海根，虞志英，钮建定，李身铎，郑建朝. 长江口横沙浅滩及邻近海域含沙量与沉积物特征分析[J]. 华东师范大学学报(自然科学版), 2013, 2013(4): 42-54.
[10]	于江江, 张健, 郑小东. Pd-Ni修饰的硅纳米线电极用于非酶葡萄糖检测[J]. 华东师范大学学报(自然科学版), 2013, 2013(3): 202-208.
[11]	王蕾，祁佩时，辛明. 河道沉积物中重金属的生态修复及根际细菌的原位检测[J]. 华东师范大学学报(自然科学版), 2012, 2012(1): 1-10, 36.
[12]	陈建军;;黄民生 ;卢少勇 ;赵屹坤 ;吴芸 ;黄国忠 . 北京六湖水体和表层沉积物中氮污染特征与评价[J]. 华东师范大学学报(自然科学版), 2011, 2011(1): 12-20.
[13]	邓可;杨世伦;刘素美;张经. 长江口崇明东滩冬季沉积物水界面营养盐通量[J]. 华东师范大学学报(自然科学版), 2009, 2009(3): 17-27.
[14]	王超;闫启仑;陈红星;闫吉成;王睿睿. 端足类河蜾蠃蜚生活周期及其沉积物毒理敏感性研究[J]. 华东师范大学学报(自然科学版), 2009, 2009(3): 1-6.
[15]	周立旻;郑祥民;王辉;王晓勇;黄东锋;宋连环;任少芳. 长江中下游河流沉积物磁性特征初探[J]. 华东师范大学学报(自然科学版), 2008, 2008(6): 24-31.