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By K. Fuchs, C. Froidevaux

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Published by way of the yankee Geophysical Union as a part of the Geodynamics Series

This quantity is dedicated to fresh advances in investigating the Earth's crustal and mantle constitution, its composition and dynamics. some of the papers replicate the controversy prepared by way of the overseas Lithosphere software (ILP) throughout the Moscow foreign Geological Congress (1980). Others stem from discussions inside of one operating crew (WG-9) and one coordinating committee (CC-5) of ILP.

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And Extension of Continental Crust WINCH profile (Fig. 26, 27, and 28) show abundant diffractions and the fault may extend vertically into the mantle where dipping reflections are apparently Rifts 1983. ) In Several deep seismic reflection traverse regions of important crustal In these data a variety of features extension can be observed. In profiles extension. , 1986). The reflection data there (Fig. S. several COCORPsurveys cross various parts of the Basin and Range province of Cenozoic to Recent normal faulting.

Kaufman, D. , 1982. C. Ando, S. Klemperer, the Geology, J. Oliver, ity. Akad. Nauk. I. Davydova, seismic crustal 1068-1084, 1965. Ein Beitrag Untergrundes, zur studies, Er{orschung Geologische des Rundschau, S. Kaufman,B. Czuchra,T. W. Isachsen, Adirondack-Appalachian crustal struc- 46, 17-26, 1957. , andK. Fuchs,Statistical evaluationof Soc. , 94, 1173-1184,1983. , M. Barazangi, S. Kaufman, and J. Oliver, The First Decadeof COCORP' 1974-1984, in Reflection Seismology' A Global Perspec- 32, 951-967, 1967.

26. Note Outer Isles Thrust (OIT) and Flannan Thrust (FT) as seen on MOIST (Figs. 24 and 25) and good reflections from Moho. NLB=North Lewis Basin, McBride across et the al, Great in Glen MB=Minch Basin. review). , 1983). and Extension of Continental Crust WINCH profile (Fig. 26, 27, and 28) show abundant diffractions and the fault may extend vertically into the mantle where dipping reflections are apparently Rifts 1983. ) In Several deep seismic reflection traverse regions of important crustal In these data a variety of features extension can be observed.

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