The Puncoviscana trough — a large basin of Late Precambrian to Early Cambrian age on the pacific edge of the Brazilian shield

[1]  H. Miller,et al.  Structural Division and Evolution of the Lower Paleozoic Basement in the NW Argentine Andes , 1986 .

[2]  H. Miller,et al.  Deposition and Facies Distribution of Turbiditic Sediments of the Puncoviscana Formation (Upper Precambrian - Lower Cambrian) within the Basement of the NW Argentine Andes , 1986 .

[3]  E. A. O'Connor,et al.  Recognition of an Eocambrian Orogenic Cycle in SW Brazil and SE Bolivia , 1986 .

[4]  H. Miller,et al.  Isotopic Dating of Polymetamorphic Metasediments from Northwest Argentina , 1986 .

[5]  H. J. Lippolt,et al.  Acid Magmatites of the Brasiliano Cycle in East Paraguay , 1986 .

[6]  F. Aceñolaza,et al.  Upper Precambrian–Lower Cambrian biota from the northwest of Argentina , 1986, Geological Magazine.

[7]  H. Miller,et al.  Geochemical features of an Upper Precambrian - Lower Cambrian greywacke/pelite sequence (Puncoviscana trough) from the basement of the NW-Argentine Andes , 1985 .

[8]  F. Aceñolaza,et al.  The trace fossil Oldhamia - Its interpretation and occurrence in the Lower Cambrian of Argentina , 1985 .

[9]  W. Zeil,et al.  Geodynamic and magmatic stages on a traverse through the Andes between 20° and 24°S (N Chile,S Bolivia, NW Argentina) , 1984, Journal of the Geological Society.

[10]  H. Miller.  Orogenic development of the Argentinian/Chilean Andes during the Palaeozoic , 1984, Journal of the Geological Society.

[11]  K. Pickering.  Transitional submarine fan deposits from the late Precambrian Kongsfjord Formats submarine fan, NE Finnmark, N. Norway , 1983 .

[12]  W. H. Fritz,et al.  Strata and trace fossils near the precambrian-cambrian boundary, Mackenzie, Selwyn and Wernecke Mountains, Yukon and Northwest Territories: reply , 1983 .

[13]  J. P. Berrangé.  THE EASTERN BOLIVIA MINERAL EXPLORATION PROJECT PROYECTO PRECÁMBRICO , 1982 .

[14]  F. Hervé,et al.  Geochronology of the pre-Andean metamorphism and magmatism in the Andean Cordillera between latitudes 30° and 36°S , 1982 .

[15]  H. Miller,et al.  Early Paleozoic orogeny in southern South America , 1982 .

[16]  F. Tessensohn.  Significance of late Precambrian turbidite sequences bordering the East Antarctic Shield , 1982 .

[17]  H. Hofmann.  First record of a Late Proterozoic faunal assemblage in the North American Cordillera , 1981 .

[18]  G. Ghibaudo.  Deep-sea fan deposits in the Macigno Formation (Middle-Upper Oligocene) of the Gordana Valley, Northern Apennines, Italy , 1981 .

[19]  B. Dalmayrac,et al.  La chaine hercynienne d'amerique du sud structure et evolution d'un orogene intracratonique , 1980 .

[20]  P. Cobbold,et al.  Structure, metamorphism an geochronology of the Arequipa Massif of coastal Peru , 1979, Journal of the Geological Society.

[21]  J. Ozard,et al.  Reconnaissance geochronology of the crystalline basement rocks of the Coastal Cordillera of southern Peru , 1977 .

[22]  Y. Hasui,et al.  The Upper Precambrian of South America , 1976 .

[23]  F. L. Schwab.  Framework mineralogy and chemical composition of continental margin-type sandstone , 1975 .

[24]  K. Crook.  Lithogenesis and Geotectonics: The Significance of Compositional Variation in Flysch Arenites (Graywackes) , 1974 .

[25]  U. Cordani,et al.  The precambrian evolution of South America , 1973 .

[26]  Raymond Siever,et al.  Sand and sandstone , 1972 .