Decompression and high-temperature-low-pressure metamorphism in the exhumed floor of an extensional basin, Alboran Sea, western Mediterranean

Leg 161 of the Ocean Drilling Program (ODP) has made a major contribution to our understanding of the origin of the Alboran Basin by demonstrating that it is underlain by rocks of continental origin that have undergone high-temperature metamorphism and melting at exceptionally low pressure after exh...

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Bibliographic Details
Published in:Geology (Boulder) 1996-05, Vol.24 (5), p.447-450
Main Authors: Platt, J. P, Soto, J. I, Comas, M. C, Zahn, R, Klaus, A, Aubourg, C, Bernasconi, S, Belanger, P, Cornell, W, de Kaenel, E, de Larouzière, F, Doose, H, Fukusawa, H, Hobart, M, Iaccarino, S, Ippach, P, Marsaglia, K, Meyers, P, Murat, A, O'Sullivan, G, Prassad, M, Siesser, W, Skilbeck, C. G, Tandon, K, Torii, M, Tribble, J, Wilkens, R
Format: Article
Language:English
Subjects:
Alboran Sea
basement
basins
bathymetry
cores
crust
crustal thinning
decompression
dikes
exhumation
extension tectonics
geologic barometry
geologic thermometry
Geology
geophysical methods
geophysical surveys
Geophysics
gneisses
granites
high temperature
high-grade metamorphism
igneous and metamorphic rocks
igneous rocks
intrusions
Leg 161
low pressure
Marine
Mediterranean Sea
metamorphic rocks
metamorphism
migmatites
mineral assemblages
Ocean Drilling Program
ocean floors
Oceanography
ODP Site 976
P-T conditions
Petrology
Plate tectonics
plutonic rocks
pressure
schists
seismic methods
solid Earth (tectonophysics)
surveys
tectonics
temperature
West Mediterranean
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Summary:Leg 161 of the Ocean Drilling Program (ODP) has made a major contribution to our understanding of the origin of the Alboran Basin by demonstrating that it is underlain by rocks of continental origin that have undergone high-temperature metamorphism and melting at exceptionally low pressure after exhumation and decompression. Basement rocks recovered from Site 976 consist of high-grade schist and gneiss derived from aluminous sediments, and minor amounts of marble, granitic dikes, and migmatitic segregations of granitic material. Mineral assemblages and textural relations show that an early assemblage including biotite, garnet, staurolite, plagioclase, and rutile is overprinted by a second assemblage of biotite, sillimanite, plagioclase, potassium feldspar, and ilmenite. Both assemblages are overprinted by andalusite, potassium feldspar, and minor garnet. Migmatitic gneiss contains relict andalusite, overprinted by sillimanite and cordierite coexisting with granitic leucosome. Preliminary pressure-temperature estimates suggest that the metamorphic evolution followed an approximately isothermal decompression path from 7 to 3 kbar at temperatures in the range 580 to 630 °C. After decompression, granitic melts formed at 670 °C, after andalusite breakdown and within the sillimanite stability field. The cored rocks closely resemble high-grade metamorphic rocks in the adjacent Betic Cordillera of southern Spain, which yield early Miocene radiometric dates. At ODP Site 976 they are overlain by middle Miocene marine sediments. The combination of exhumation in an extensional tectonic environment and the evidence for high and increasing temperature during exhumation provide support for and new constraints on current models for the basin that involve the removal of lithospheric mantle below a zone of continental collision, accompanied or followed by extension.
ISSN:0091-7613
1943-2682
DOI:10.1130/0091-7613(1996)024<0447:DAHTLP>2.3.CO;2