Kerguelen hotspot magma output since 130 Ma

被引:370
作者
Coffin, MF
Pringle, MS
Duncan, RA
Gladczenko, TP
Storey, M
Müller, RD
Gahagan, LA
机构
[1] Univ Tokyo, Ocean Res Inst, Nakano Ku, Tokyo 1648639, Japan
[2] Japan Marine Sci & Technol Ctr, Inst Frontier Res Earth Evolut, Yokosuka, Kanagawa 2370061, Japan
[3] Univ Texas, Inst Geophys, Jackson Sch Geosci, Austin, TX 78759 USA
[4] Scottish Univ Environm Res Ctr, E Kilbride G75 0QF, Lanark, Scotland
[5] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[6] Dynam Graph Inc, Alameda, CA 94501 USA
[7] Danish Lithosphere Ctr, DK-1350 Copenhagen, Denmark
[8] Univ Sydney, Sch Geosci, Div Geol & Geophys, Sydney, NSW 2006, Australia
关键词
hotspot; mantle plume; large igneous province; flood basalt; Kerguelen Plateau;
D O I
10.1093/petrology/43.7.1121
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 Kerguelen hotspot (Indian Ocean) has produced basalt for similar to130 Myr, among the longest known volcanic records from a single source. New and published 40Ar/39Ar age determinations from the Kerguelen Plateau, Broken Ridge, Rajmahal Traps, and Bunbury basalts, and of Indian and Antarctic dikes help to document the hotspot's history. Using radiometric dates and crustal structure determined from geophysical data and drilling results, we calculate the magmatic output of the Kerguelen hotspot through time. Output rates have varied in ways not predicted by current geodynamic models; maximum eruption volumes postdate the initial surface manifestation of the hotspot as well as break-up between Antarctica and India by greater than or equal to15 Myr, and magma output rates were high, as well as geographically diverse, over an interval of 25 Myr, from similar to120 to similar to95 Ma. We propose two alternatives to the standard mantle plume paradigm, one involving multiple plume sources, and another consisting of a single, but dismembered plume source.
引用
收藏
页码:1121 / 1139
页数:19
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