Magnetic and bathymetric investigations over the Vema Region of the Central Indian Ridge: tectonic implications

被引:13
作者
Drolia, RK
Ghose, I
Subramanyam, AS
Rao, MMM
Kessarkar, P
Murthy, KSR
机构
[1] Natl Geophys Res Inst, Hyderabad 500007, Andhra Pradesh, India
[2] Natl Inst Oceanog, Geol Oceanog Div, Panaji 403004, Goa, India
[3] Reg Ctr, Natl Inst Oceanog, Visakhapatnam 530017, Andhra Pradesh, India
关键词
Central Indian Ridge; mid-ocean tectonics; marine magnetic anomalies; Vema Fracture Zone;
D O I
10.1016/S0025-3227(00)00029-3
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Magnetic and bathymetric data were collected along N50 degrees E profiles in the Vema Region (7-12 degrees S, 64-70 degrees E) across five ridge segments of the Central Indian Ridge (CIR). Anomalies up to A5 (10 Ma), identified by generating synthetics for each profile, show asymmetric spreading. Though inter-segmental variations in spreading rate have been observed, the mean half-spreading rate increases from 1.8 cm/yr in the region north of Vema Transform to 2.1 cm/yr south of the Vema Transform. The average spreading rate for the last 10 Ma has not always been symmetric. The interpretation of magnetic and bathymetric data shows the complex nature of this part of the CLR which could probably be attributed to: (i) the short ridge segment; (ii) interaction with Fracture zone; and (iii) interaction between the CIR and the Wide Boundary Zone (WBZ) separating the Indian and Australian plates. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:413 / 423
页数:11
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