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Mesozoic Troughs and Crustal Structure in Anatolia
Geological Society of America Bulletin, 1972In Anatolia, zones of ultramafic masses were emplaced during the Mesozoic into the upper crustal level. Along these zones, deep-sea troughs, characterized by radiolarite-ophiolite facies, developed within the shallow Tethys sea. After some time, the troughs were filled by mafic volcanic rocks and abyssal sediments.
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Truncated crustal transfer functions and fine crustal structure determination
Bulletin of the Seismological Society of America, 1967abstract A seismic pulse is influenced by the various media through which it has travelled. The crust is known to have a considerable influence. With the use of the Thomson-Haskell matrix formulation, the crustal effect can be easily calculated.
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Crustal Structure of Western Portugal
1983Abstract Crustal investigations of Western Portugal, along the Mesozoic zone situated between Lisboa and Nazare, show the following major characteristics: in the uppermost 8 km the velocity increases continuously with increasing depth reaching the unusually high value of 6.5 km/s; this layer is underlain by a sialic low-velocity layer, probably ...
V.S. MOREIRA +3 more
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Crustal structure of the Indian subcontinent
Tectonophysics, 1973Abstract Studies carried out by various investigators up to 1971 to delineate the Indian crustal structure using body wave travel times, surface wave dispersion and gravity methods are summarised and reviewed. The average crustal thickness is found to be 35–40 km in the Indian peninsular shield, 30–35 km in the Indo Gangetic plains and 60–80 km in ...
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Synthesis of Oceanic Crustal Structure From Two‐Dimensional Seismic Profiles
Reviews of Geophysics, 2019Gail L Christeson +2 more
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