Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

C Ishwar-Kumar, K Sajeev, BF Windley, TM Kusky… - Tectonophysics, 2015 - Elsevier
The occurrence of high-pressure mafic–ultramafic bodies within major shear zones is one of
the indicators of paleo-subduction. In mafic granulites of the Andriamena complex (north …
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[引用][C] Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

C Ishwar-Kumar, K Sajeev, BF Windley, TM Kusky… - Tectonophysics, 2015 - cir.nii.ac.jp
Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic
implications | CiNii Research CiNii 国立情報学研究所 学術情報ナビゲータ[サイニィ] 詳細へ移動 …

Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

C Ishwar-Kumar, K Sajeev, BF Windley… - …, 2015 - ui.adsabs.harvard.edu
The occurrence of high-pressure mafic-ultramafic bodies within major shear zones is one of
the indicators of paleo-subduction. In mafic granulites of the Andriamena complex (north …

Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

C Ishwar-Kumar, K Sajeev, BF Windley… - …, 2015 - eprints.iisc.ac.in
The occurrence of high-pressure mafic-ultramafic bodies within major shear zones is one of
the indicators of paleo-subduction. In mafic granulites of the Andriamena complex (north …
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[PDF][PDF] Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

C Ishwar-Kumar, K Sajeev, BF Windley, TM Kusky… - 2015 - drive.google.com
The occurrence of high-pressure mafic-ultramafic bodies within major shear zones is one of
the indicators of paleo-subduction. In mafic granulites of the Andriamenaa complex (north …

Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

C Ishwar-Kumar, K Sajeev, BF Windley, TM Kusky… - Tectonophysics, 2015 - infona.pl
The occurrence of high-pressure mafic–ultramafic bodies within major shear zones is one of
the indicators of paleo-subduction. In mafic granulites of the Andriamena complex (north …

Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

C Ishwar-Kumar, K Sajeev, BF Windley… - …, 2015 - eprints.iisc.ac.in
The occurrence of high-pressure mafic-ultramafic bodies within major shear zones is one of
the indicators of paleo-subduction. In mafic granulites of the Andriamena complex (north …