FORMATION OF MARGINAL BASINS AND ITS IMPLICATION TO THE TECTONIC EVOLUTION OF SOUTHEAST CHINA
Received date: 1996-06-07
Revised date: 1996-07-01
Online published: 1997-02-01
Although a large variety of mechanisms have been proposed to account for the formation of marginal basins, including “entrapment” origin, back arc spreading and intraplate stress propogation, etc., no solution has ever reached for the formation and evolution for marginal basins in the western Pacific. The study of marginal basins should take into account the mechanisms for continental deformation, thus constitute a 3-D approach to the problem. Recent contributions in the study of marginal basins also shed new light in the study of tectonic evolution of Southeast China. Cautions should be taken in the identification of ancient volcanic arcs, subduction zones and the reconstruction of ocean basins. The combined effect of NNE trending transform faults related to Paleo tethys and the movement of Paleo Pacific plates play a significant role in the formation of huge Mesozoic igneous activities. Transition from transform fault to subduction system constitutes a unique form of continental accretion for Southeast China and its adjacent areas. Sediment record in the related basins will provide substantial information for the related continental collision and mountain building and erosion process.
ZHOU Zuyi, DING Xiao, LIAO Zongting, JIN Xingchun . FORMATION OF MARGINAL BASINS AND ITS IMPLICATION TO THE TECTONIC EVOLUTION OF SOUTHEAST CHINA[J]. Advances in Earth Science, 1997 , 12(1) : 7 -14 . DOI: 10.11867/j.issn.1001-8166.1997.01.0007
1 Karig D E.Origin and development of marginal basins in the western Pacific. J Geophys Res,1971,76:2542-2561.
2 Ben-Avraham Z, Uyeda S.Entrapment of marginal seas. In:Hilde T W C, et al(eds). Geodynamics of the Western Pacific-Indonesian Region. Geodynamic Series,1983,II:91-104.
3 Hilde T W C,Lee C S. Origin and evolution of the West Philippine basin: a new interpretation. Tectonophysics,1984,102:85-104.
4 Uyeda S, Kanamori K. Back-arc opening and the mode of subduction.J Geophys Res,1979,84:1049-1061.
5 Carlson R L, Melia P J. Subduction hinge migration. Tectonophysics,1984,102:399-411.
6 Sleep N H, Toksoz M N. Evolution of marginal basins. Nature,1971,33:548-550.
7 Tatsumi Y,Otofuji Y I,Matsuda T, Nohda S.Opening of the Sea of Japan back-arc basin by asthenospheric injection.Tectonophysics,1989,166:317-329.
8 Miyashiro A. Hot regions and the origing of marginal basins in the Western Pacific. Tectonophysics,1986,122:195-216.
9 Charvet J, Ogawa Y. Arc-trench tectonics. In: Hancock P L(ed). Continental Deformation. Pergamon Press,1994.184-199.
10 Viallon C, Huchon P, Barrier E. Opening of the Okinawa basin and the collision in Taiwan: A retreating trench model with lateral anchoring. Earth Planetary Science Letters,1986,80:145-155.
11 Letouzey J, Kimura M.Okinawa Trough genesis: structure and evolution of a bach-arc basin model developed in a continent. Mar Petro Geol,1985,2:111-130.
12 Zhou Z. The early Mesozoic orogeny in the northern shelf of the South China Sea and its adjacent lands. In:Jin X L et al.(eds).Marine Geology and Geophysics of the South China Sea. China Ocean Press,1992.119-125.
13 Ben-Avraham Z. Multiple opening and closing of the eastern Mediterranean and South China basins. Tectonics,1989,8(2):351-362.
14 Lao Q, Zhu X. Geological history of the marginal seas of China. In: Wang P et al. (eds). Asian Marine Geology.China Ocean Press,1990.63-72.
15 Mason R. Did the Iapetus Ocean really exist? Geology,1988,16:823-826.
16 Sengor A M C. Plate tectonics and orogeny research after 25 years: a Tethyan perspective. Earth-Science Reviews,1990,27:1-201.
17 Pearce J A, Lippard S J, Roberts S. Characteristics and tectonic significance of supra-subduction zone ophiolites.In: Kokelaar B P et al.(eds).Marginal Basin Geology. Blackwell Scientific Publications.1984.
18 朱夏.中国大陆边缘构造和盆地演化.石油实验地质,1982,4(3):1-7.
19 王鸿桢.中国华南地区地壳发展的轮廓.见:王鸿桢主编.华南地区古大陆边缘构造史.武汉地质学院出版社,1986,1-15.
20 Zhou Z, Lao Q, Chen H, et al. Early Mesozoic orogeny in Fujian, SE China.In: R Hall et al.(eds). Tectonic Evolution of Southeast Asia, Geological Society Special Publication(106):549-556.
21 姚伯初,曾维军,陈艺中,等.南海西沙海槽:一条古缝合线.海洋地质与第四纪地质,1994,14(1):1-10.
22 Maruyama S, Seno T. Orogeny and relative plate motions: example of Japanese islands. Tectonophysics,1986,127:305-329.
23 张用夏.华南地区中生代岩浆活动与地幔热源的关系.南京地矿所所刊,1986,7(4):53-64.
24 郭令智,施央申,卢华复,等.中国南部地体构造的研究.南京大学学报,1984,26(4):732-737.
25 王鸿桢,杨森楠,李思田.中国东部及邻区中、新生代盆地发育及其大陆边缘的构造发展.地质学报,1983,57(3):213-223.
26 周祖翼.闽东沿海构造带.见:刘光鼎主编.中国海区及领域地质地球物理特征.北京:科学出版社,1992.320-326.
27 莫柱荪.南岭地区陆壳的生长和花岗岩的演化.第二届全国构造地质学术会议论文集(第一卷).北京:地质出版社,1981.
28 林瑶珉.福建沿海A型花岗岩的基本特征及其大地构造意义.大地构造与成矿学,1987,11(5):196-201.
29 Otsuki K. Plate tectonics of Eastern Eurasia in the light of fault systems. Science Report of the Tohoku University,2nd Series(geology),1985,55(2):251.
30 Engebreston D C, Cox A, Gordon R G. Relative motions between oceanic and continental plates in the Pacific basin.Geol Soc Am Spec Pap,1985:55.
31 Charvet J, Faure M, Caridroit M, Guidi A. Some tectonic and tectogenetic aspects of SW Japan: an Alpine-typorogen in an island-arc position. In: Nasu N et al. (eds). Active Ocean Margins.TERRAPUB,Tokyo,1985:791-817.
32 Covey M. The evolution of foreland basins to steady state: evidence from the western Taiwan foreland basins.In:Allen P A et al. (eds).Foreland Basins.Blackwell Scientific Publications,1986.77-99.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
