Petrogenesis of the Dalongkai ultramafic-mafic intrusion and its tectonic implication for the Paleotethyan evolution along the Ailaoshan tectonic zone (SW China)
© 2016 Elsevier Ltd.Layered ultramafic-mafic intrusions are usually formed in an arc/back-arc or intra-plate tectonic environment, or genetically related to a mantle plume. In this paper, we report on an ultramafic-mafic intrusion, the Dalongkai intrusion in the Ailaoshan tectonic zone (SW China), w...
| Main Authors: | , , |
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| Format: | Journal Article |
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Pergamon-Elsevier Science Ltd
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/51044 |