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Timing, quantification and tectonic modelling of Pliocene-Quaternary movements in the NW Himalaya: evidence from fission track dating
Jaina, A.K.; Kumarb, D.; Singha, S.; Kumarc, A.; Lalc, N.
Petrogenetic significance of ferro-enstatite orthopyroxene in basaltic dikes from the Tapi rift, Deccan flood basalt province, India
Chandrasekharama, D.; Vasellib, O.; Shethc, H.C.; Keshavd, S.
Metal-silicate interaction in quenched shock-induced melt of the Tenham L6-chondrite
Lerouxa, H.; Doukhana, J.; Guyotb, F.
Evidence for Early Cretaceous oceanic crust trapped in the Philippine Sea Plate
deschampsa, A.; Moniea, P.; Lallemanda, S.; Hsub, S.; Yehc, K.Y.
Evidence for a 20o tilting of the Earth's rotation axis 110 million years ago
Prevot, M.; Mattern, E.; Camps, P.; Daignieres, M.
The Mid-Pleistocene climate transition as documented in the deep South Atlantic Ocean: initiation, interim state and terminal event
Schmieder, F.; von Dobeneck, T.; Bleil, U.
Seismic anisotropy of South African upper mantle xenoliths
Long, C.; Christensen, N.I.
Comment on ''Crustal structure based on gravity-magnetic modelling constrained from seismic studies under Lambert Rift, Antarctica and Godavari and Mahanadi rifts, India and their interrelationship'' by D.C. Mishra et al.
Reply to the comments by S.K. Acharyya on ''Crustal structure based on gravity-magnetic modelling constrained from seismic studies under Lambert Rift, Antarctica and Godavari and Mahanadi rifts, India and their interrelationship''
Mishra, D.C.; Chandrasekhar, D.V.; Ventata Raju, D.C.; Vijaya Kumar, V.
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