Petrology of ultramafic rocks at DSDP Holes 82-556, 82-558, and 82-560
Strongly serpentinized peridotites occur at shallow crustal levels at DSDP Sites 556 (35-Ma-old crust), 558 (35-Maold crust), and 560 (12-Ma-old crust) in the North Atlantic. Primary peridotite silicate minerals are preserved only at Sites 556 and 558, but all three sites have primary spinel preserv...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
1985
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.806240 https://doi.org/10.1594/PANGAEA.806240 |