Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol19.Issue1-2.Feb2001:
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The ¯attening strain adjacent to the MCT and the crystalline klippen changes to either plane strain or constrictional strain and this zone is dominated by S±C microstructures.. Such
Because volcaniclastic sediments are absent in the adja- cent, structurally underlying crustal and mantle sequences (the ophiolite component) of the Neyriz ophiolite complex, we
T.N. Representative EPMA backscatter images of zircons from the granulite complex of the Kontum massif. Positions of spots of SHRIMP U±Pb analyzing are shown.. granulites of
A crustal shear zone in the interface zone between the Higher and Lesser Garhwal Himalaya with considerably high P-wave velocity and pronounced seismic activity is identi®ed. In
Two formation mechanisms have been postulated: the `precipitation' model for the sagenitic biotite of igneous origin (Shau, Y.H., Yang, H.Y., Peacor, D.R., 1991. On oriented
Age of the Sungai Bera section brachiopods and possible correlation with other horizons in the Central Basin of Peninsular Malaysia, the Sisophon Limestone of west Cambodia, and
The strata exposed on the northern ¯ank of the anticline along the coast are designated as the Tsuku Formation, whereas no corresponding stratum is shown to the south of the
The ®nal exhumation of the Song Chay orthogneiss constrained by ®ssion-track analysis on samples along the same transect occurred during the Early Miocene and could be interpreted
