By H. Berckhemer, K. Hsü
About The Product
Published through the yank Geophysical Union as a part of the Geodynamics Series.
The ultimate file on geodynamic study within the Alpine-Mediterranean sector will be incomplete with no short ancient comic strip at the constitution and actions of ICG-Working crew three. it's going to even be appeared an appreciation to the individuals and sponsors of the operating workforce who've taken, over decades, an energetic half within the lifetime of the operating staff and thereby contributed to the outstanding development in our wisdom and figuring out of the geological evolution of this complicated area.
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Additional info for Alpine-Mediterranean Geodynamics
Rifting and subsidence of the western continental margin of the Bay of Biscay. Initial Rep. Deep Sea drill. ,48, 1025-1060, 1979. M. , The Troodos Massif, Cyprus and other ophiolites as oceanic crust: evaluation and implications. Phil. Trans. R. Soc. London, A268, 433-466, 1971. H. , The Ocean Basins and Margins, Volume 4A, The Western Mediterranean, Plenum Press, New York and London, 1977. H. , The Ocean Basins and Margins, Volume 4B, The Eastern Mediterranean, Plenum Press, New York and London, 1978.
Verh. K. Ned. geol. mijnboukwd. , 1-423, 1974. 31, in Geol. , 108, 1971. Waters, Romania. J. , Bull. •eol. Soc. , 85, 1429-1440, 1974. Horvath, F. , Further evidence relevant to the African/Adriatic promontory as a palaeogeographic premise for Alpine orogeny. In Biju-Duval, B. & Montadert, L. (eds) 'Structural history of the Mediterranean basins', Editions Technip, Paris, 133-142, 1977. J. The meaning historical search. 7, 1-11, of the word flysch; a short Geol. Ass. Can. Spec. , 1970. , Origin Mediterranean.
Smith  pointed out the need to seek the Africa • Fig. 18. The original surrounding continents Fig. 31b]. I shape of the Tethys and according to Carey [1958, TECTONIC Copyright American Geophysical Union SYNTHESES 29 Geodynamics Series Alpine-Mediterranean Geodynamics Mesozoic carbonate platforms of the circumMediterranean region all lay south of the Mesozoic Tethys and represent deposits on its southern continental margin. By contrast with eastern North America, the passive continental margin deposits of Morocco have been uplifted and exposed.
Alpine-Mediterranean Geodynamics by H. Berckhemer, K. Hsü