If you are experiencing problems downloading PDF or HTML fulltext, our helpdesk recommend clearing your browser cache and trying again. If you need help in clearing your cache, please click here . Still need help? Email firstname.lastname@example.org
< previous issue
next issue >
Early tectonic dewatering and brecciation on the overturned sequence at Marble Bar, Pilbara Craton, Western Australia: dome-related or not?
Oliver, N.H.S.; Cawood, P.A.
Nd isotope and petrogenetic constraints for the origin of the Mount Angelay igneous complex: implications for the origin of intrusions in the Cloncurry district, NE Australia
Evidence for 1.82 Ga transpressive shearing in a 1.85 Ga granitoid in central Sweden: implications for the regional evolution
Hogdahl, K.; Sjostrom, H.
Marine evaporites from an oceanic island in the Neoproterozoic Adamastor ocean
Frimmel, H.E.; Jiang, S.
Comment on ''Evidence for multiphase deformation in the Archaean basal Warrawoona group in the Marble Bar area, East Pilbara, Western Australia'' by van Haaften, W.M., White, S.H., 1998 - Precambrian Research 88, 53-66
van Kranendonk, M.J.; Hickman, A.H.; Collins, W.J.
Reply to comment on ''Evidence for multiphase deformation in the Archaean basal Warrawoona group in the Marble Bar area, East Pilbara, Western Australia'' (van Haaften, W.M., White, S.H., 1998. Precambrian Research 88, 53-66) by M.J., Van Kranendonk, A.H. Hickman, W.J., Collins
van Haaften, W.M.; White, S.H.
15N-depleted nitrogen in Early Archean kerogens: clues on ancient marine chemosynthetic-based ecosystems? - A comment to Beaumont, V., Robert, F., 1999. Precambrian Res. 96, 62-82
Pinti, D.L.; Hashizume, K.