By H. Berckhemer, K. Hsü
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Published via the yank Geophysical Union as a part of the Geodynamics Series.
The ultimate document on geodynamic study within the Alpine-Mediterranean zone will be incomplete and not using a short ancient comic strip at the constitution and actions of ICG-Working team three. it may even be looked an appreciation to the contributors and sponsors of the operating workforce who've taken, over a long time, an lively half within the lifetime of the operating team and thereby contributed to the notable growth in our wisdom and knowing of the geological evolution of this complicated zone.
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Concerning the ProductPublished by means of the yankee Geophysical Union as a part of the Geodynamics sequence. the ultimate file on geodynamic study within the Alpine-Mediterranean zone will be incomplete with no short old caricature at the constitution and actions of ICG-Working crew three. it's going to even be appeared an appreciation to the contributors and sponsors of the operating team who've taken, over a long time, an energetic half within the lifetime of the operating staff and thereby contributed to the striking growth in our wisdom and realizing of the geological evolution of this advanced quarter.
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Additional info for Alpine-Mediterranean Geodynamics
Palaeontol. 12, 1-42, 1973. M.
Geol. Soc. , 85, 1077-1083, 1974. P. , Gravity anomalies, ultramafic intrusions and the tectonics of the region around the Strait of Gibraltar. J. geophys. , 78, 1371-1382, 1973. Bosellini, A. , Mediterranean plate tectonics and Triassic palaeogeography. Nature London, 244, 144-146, 1973. , Le probleme de l'origine des nappes et de leurs translations cidentales. Bull. 101-106, 1974. , of the dans Soc. geol. E. , The Atlantic. Philos. Trans. R. Soc. London, A258, 41-51, 1965. , The geology of Romania.
In press]. Note the much reduced size of the Tethys. C=Caribbean, I=Italy, G=Greece, T=Turkey. The positions of C,I,G and T are entirely speculative. The transition from this figure to the late Triassic reconstruction of Fig. 16 can be made by a transform zone lying on the northern edge of Gondwanaland. g. g. g. McKenzie, 1977]. It is worth noting that all the continental areas in the region that are today deforming 'plastically', or have recently ceased to deform plastically, are all located in areas affected by earlier subduction and within a few hundred kilometers of the in- ferred surface trace of the subduction zone.
Alpine-Mediterranean Geodynamics by H. Berckhemer, K. Hsü