Chemical and strontium isotopic investigations of ultramafic inclusions and basalt, Bandera Crater, New Mexico

Details Chemical and strontium isotopic investigations of ultramafic inclusions and basalt, Bandera Crater, New Mexico Chemical and strontium isotopic investigations of ultramafic inclusions and basalt, Bandera Crater, New Mexico

Jan 1971

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1971gecoa..35..107l&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 35, Issue 1, pp.107-113

Physics

7

Scientific paper

A new locality for lherzolite inclusions in basalt has been found in a
cinder eruption of Bandera Crater, New Mexico. Red-spinel lherzolites
had 87 Sr / 88 Sr ratios of 0.7045-0.7055, green-spinel lherzolites
0.7023-0.7040 and basalt 0.7028-0.7034. The red spinel lherzolites
apparently have no genetic relationship to the basalt.

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