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Large igneous provinces: crustal structure, dimensions, and external consequences
Citation
Coffin, MF and Eldholm, O, Large igneous provinces: crustal structure, dimensions, and external consequences, Reviews of Geophysics, 32, (1) pp. 1-36. ISSN 8755-1209 (1994) [Refereed Article]
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Copyright Statement
Copyright Statement: Copyright 1994 by the American Geophysical Union Official URL Field: http://www.agu.org/
Abstract
Large igneous provinces (LIPs) are a continuum
of voluminous iron and magnesium rich rock
emplacements which include continental flood basalts
and associated intrusive rocks, volcanic passive margins,
oceanic plateaus, submarine ridges, seamount
groups, and ocean basin flood basalts. Such provinces
do not originate at "normal" seafloor spreading centers.
We compile all known in situ LIPs younger than
250 Ma and analyze dimensions, crustal structures,
ages, and emplacement rates of representatives of the
three major LIP categories: Ontong Java and Kerguelen-
Broken Ridge oceanic plateaus, North Atlantic
volcanic passive margins, and Deccan and Columbia
River continental flood basalts. Crustal thicknesses
range from 20 to 40 km, and the lower crust is characterized
by high (7.0-7.6 km s -1 compressional
wave velocities. Volumes and emplacement rates derived
for the two giant oceanic plateaus, Ontong Java
and Kerguelen, reveal short-lived pulses of increased
global production; Ontong Java's rate of emplacement
may have exceeded the contemporaneous global production rate of the entire mid-ocean ridge system. The
major part of the North Atlantic volcanic province lies
offshore and demonstrates that volcanic passive margins
belong in the global LIP inventory. Deep crustal
intrusive companions to continental flood volcanism
represent volumetrically significant contributions to
the crust. We envision a complex mantle circulation
which must account for a variety of LIP sizes, the
largest originating in the lower mantle and smaller
ones developing in the upper mantle. This circulation
coexists with convection associated with plate tectonics,
a complicated thermal structure, and at least four
distinct geochemical/isotopic reservoirs. LIPs episodically
alter ocean basin, continental margin, and continental
geometries and affect the chemistry and physics
of the oceans and atmosphere with enormous
potential environmental impact. Despite the importance
of LIPs in studies of mantle dynamics and global
environment, scarce age and deep crustal data necessitate
intensified efforts in seismic imaging and scientific
drilling in a range of such features.
Item Details
Item Type: | Refereed Article |
---|---|
Keywords: | large igneous provinces, LIPs, massive crustal emplacements, mafic, volcanism, mantle circulation |
Research Division: | Earth Sciences |
Research Group: | Geology |
Research Field: | Marine geoscience |
Objective Division: | Expanding Knowledge |
Objective Group: | Expanding knowledge |
Objective Field: | Expanding knowledge in the earth sciences |
UTAS Author: | Coffin, MF (Professor Mike Coffin) |
ID Code: | 73827 |
Year Published: | 1994 |
Web of Science® Times Cited: | 1139 |
Deposited By: | Research Division |
Deposited On: | 2011-10-26 |
Last Modified: | 2013-03-06 |
Downloads: | 21 View Download Statistics |
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