Geodynamic implications of moving Indian Ocean hotspots

被引:80
作者
O'Neill, C
Müller, D
Steinberger, B
机构
[1] Univ Sydney, Sch Geosci, Sydney, NSW 2006, Australia
[2] JAMSTEC, IFREE, Yokosuka, Kanagawa 2370061, Japan
关键词
hotspot; Indian Ocean; intraplate volcanics; plate reconstruction; paleolatitude; plume;
D O I
10.1016/S0012-821X(03)00368-6
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The reconstructed positions of many of the Indian Ocean intraplate volcanic features are inconsistent with the present positions of the hotspots to which they have been ascribed. The discrepancy can be explained by the past motion of the hotspots themselves, and in the errors introduced in an absolute plate model based on fixed hotspots. Previous models for the motion of hotspots in the Indian Ocean (e.g. [Steinberger and O'Connell, in: The History and Dynamics of Global Plate Motions, 2000, pp. 377-398, and Geophys. J. Int. 132 (1998) 412-434; Antretter et al., Earth Planet. Sci. Lett. 203 (2002) 635-650]) have had success in matching paleolatitudes of the Kerguelen hotspot, but not the Marion or Reunion hotspots. We calculate the motion of the Indian Ocean hotspots using a method described in Steinberger and O'Connell (op. cit.), employing a plate motion model revised using identification of Mesozoic magnetic anomalies in the Enderby Basin [Gaina et al., in: The Evolution and Dynamics of the Australian Plate, in press]. We find a motion of similar to7degrees south for the Kerguelen plume, similar to previous models [Antretter et al., op. cit.]. This motion alleviates the discrepancies in the position of the Kerguelen plume and its purported involvement in the formation of the Ninetyeast Ridge, RajmahaI Traps, Bunbury basalts and assorted volcanics of the Western Australian margin. We find a motion of 5degrees north and 7degrees south for the Reunion and Marion plumes, respectively. The motion of the Reunion hotspot is consistent with paleolatitude estimates. The apparent fixity of the Marion hotspot [Torsvik et al., Earth Planet. Sci. Lett. 164 (1998) 221-232] is not well-constrained, but may be due to the combination of hotspot motion and true polar wander acting in opposing directions. We present revised absolute finite rotations for the Indian plate for the last 65 Ma based on the motion of these hotspots, which place India farther north in the past than for fixed hotspot models. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:151 / 168
页数:18
相关论文
共 74 条
[1]  
[Anonymous], 1991, PROC OCEAN DRILL SCI, DOI DOI 10.2973/ODP.PROC.SR.121.162.1991
[2]   Paleolatitudes of the Kerguelen hotspot: new paleomagnetic results and dynamic modeling [J].
Antretter, M ;
Steinberger, B ;
Heider, F ;
Soffel, H .
EARTH AND PLANETARY SCIENCE LETTERS, 2002, 203 (02) :635-650
[3]  
ANTRETTER M, 2000, EGS ANN C NIC
[4]   WIDESPREAD EARLY CRETACEOUS FLOOD-BASALT VOLCANISM IN EASTERN-INDIA - GEOCHEMICAL DATA FROM THE RAJMAHAL BENGAL SYLHET TRAPS [J].
BAKSI, AK ;
BARMAN, TR ;
PAUL, DK ;
FARRAR, E .
CHEMICAL GEOLOGY, 1987, 63 (1-2) :133-141
[5]  
Barling, 1990, AM GEOPHYS UNION ANT, V48, P435
[6]   REVISED AND SYNTHETIC APPARENT POLAR WANDER PATHS OF THE AFRICAN, EURASIAN, NORTH-AMERICAN AND INDIAN PLATES, AND TRUE POLAR WANDER SINCE 200 MA [J].
BESSE, J ;
COURTILLOT, V .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1991, 96 (B3) :4029-4050
[7]   Apparent and true polar wander and the geometry of the geomagnetic field over the last 200 Myr [J].
Besse, J ;
Courtillot, V .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2002, 107 (B11)
[8]   REVISED CALIBRATION OF THE GEOMAGNETIC POLARITY TIMESCALE FOR THE LATE CRETACEOUS AND CENOZOIC [J].
CANDE, SC ;
KENT, DV .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B4) :6093-6095
[9]   ON THE STATISTICAL PROPERTIES OF ESTIMATED ROTATIONS [J].
CHANG, T .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1987, 92 (B7) :6319-6329
[10]  
CHANG T, 1988, J AM STAT ASSOC, V83, P1178