Late Paleozoic Accretionary Complexes on the Gondwana Margin of Southern Chile: Evidence from The Chonos Archipelago
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R. Pankhurst | C. Mpodozis | F. Hervé | M. Brook | E. Godoy | J. Davidson
[1] R. Pankhurst,et al. Rb‐Sr Geochronology of the Region Between The Antarctic Peninsula and The Transantarctic Mountains: Haag Nunataks and Mesozoic Granitoids , 2013 .
[2] Y. Ogawa. Variety of subduction and accretion processes in cretaceous to recent plate boundaries around Southwest and central Japan , 1985 .
[3] R. Forsythe. The late Palaeozoic to early Mesozoic evolution of southern South America: a plate tectonic interpretation , 1982, Journal of the Geological Society.
[4] C. Mpodozis,et al. The late paleozoic in chile : stratigraphy, structure and possible tectonic framework , 1981 .
[5] J. Moore. Variation in strain and strain rate during underthrusting of trench deposits , 1979 .
[6] H. Miller. Das Grundgebirge der Anden im Chonos-Archipel, Region Aisén, Chile , 1979 .
[7] D. Cowan,et al. A dynamic, scaled model of accretion at trenches and its implications for the tectonic evolution of subduction complexes , 1978 .
[8] G. Moore,et al. Development of sedimentary basins on the lower trench slope , 1976 .
[9] D. Karig. Evolution of Arc Systems in the Western Pacific , 1974 .
[10] G. Walton,et al. Trench Slope Model , 1974 .
[11] J. Stiefel. Das Andenprofil im Bereich des 45. südlichen Breitengrades , 1970 .