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Temperature gradient and structure of the lithospheric block beneath the southeastern margin of the Siberian craton: Disintegrated xenolith evidence from kimberlitic pipes of the Aldan shield
Authors: Ashchepkov, IV Vladykin, NV Gerasimov, PA Saprykin, AI Khmel'nikova, OS Anoshin, GN
Citation: Iv. Ashchepkov et al., Temperature gradient and structure of the lithospheric block beneath the southeastern margin of the Siberian craton: Disintegrated xenolith evidence from kimberlitic pipes of the Aldan shield, DOK EARTH S, 378(4), 2001, pp. 495-499
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