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vol.12 issue2A NEW APPROACH ON THE TECTONOMETAMORPHIC MECHANISMS ASSOCIATED WITH P-T PATHS OF THE BARROVIAN-TYPE SILGARÁ FORMATION AT THE CENTRAL SANTANDER MASSIF, COLOMBIAN ANDESGEOPHYSICAL PROSPECTING OF THE TRANSITION ZONE BETWEEN THE CONGO CRATON AND THE PANAFRICAN BELT IN CAMEROON author indexsubject indexarticles search
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Earth Sciences Research Journal

Print version ISSN 1794-6190

Abstract

MUSTAFIZUR RAHMAN, Syed; REZAUL ISLAM, M.; MUMNUNUL, Keramat  and  UL-ISLAM, Sultan. DEEP CRUSTAL STRUCTURE AND ESTIMATION OF MOHO IN THE LHASA TERRANE OF CENTRAL TIBET. Earth Sci. Res. J. [online]. 2008, vol.12, n.2, pp.156-168. ISSN 1794-6190.

Seismic attributes analysis is applied to INDEPTH II seismic profiles to develop a better understanding of the deep crustal structure and geodynamics of the Lhasa Terrane in the central Tibet area. Analyses indicate that the frequency anomalies are obtained over the range in between 0-30 Hz. Some area of the analyzed traces of the seismic profiles have shown dominated frequency anomaly of approximately 10 Hz with little amount of other frequencies. The variation of frequency anomaly is shown to be the indication of theMoho depth of the area. EstimatedMoho depths are found very irregular and varying from 20 kmto more than 136 km. The crust is thinner in southern, northern and eastern parts of the area while it is thicker in the western part having asymmetric nature in the central part. This variation might be the result of complicated tectonic process of the Indian and Eurasian plates. Vertically downward pocket like frequency distributions and similar type of frequency distributions at near and far depth are also observed in one of the analyzed sections. It might be indication of uprised asthenospheric matter which exchanged with lithosphere in subduction zones related to the multiple crustal uprising.

Keywords : Seismic Attributes; Central Tibet; INDEPTH; Moho; Subduction.

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