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- W2027681330 abstract "The granulite facies Highland Complex of central and southwestern Sri Lanka was thrusted onto the amphibolite facies eastern Vijayan Complex along a deep crustal, subhorizontal thrust surface. The transport direction is marked by a N-S to NNW-SSE oriented stretching lineation. During thrusting folds with axes parallel to the stretching lineation formed. Sense of shear criteria are scarce; in a few localities top to S movement is indicated. The approximately N-S oriented stretching direction is a constant element through the entire deformational history. Following thrusting the thrust contact was bent into gentle to open flexure-slip folds, which usually did not generate a new cleavage. These folds vary in wavelength between several metres and kilometres. In general their fold envelope is subhorizontal and therefore the thrust must underlie large parts of the Highland Complex. Klippen south of the Highland Complex, like the Kataragama Klippe, prove that the thrust plane is subhorizontal nearly up to the south coast, i.e. the thrust plane can be traced for more than 200 km parallel to the transport direction. After cooling to upper amphibolite facies conditions thrusting occurred during retrograde metamorphism of the Highland Complex. It is younger than the formation of 577 ± 14 Ma old migmatites (Hölzl et al., 1991). Pegmatites intruded after the formation of the thrust and are found in the Highland Complex and E-Vijayan. They were probably derived from late- to post-tectonic granitoids, which are common in the E-Vijayan. These pegmatites are not or just marginally deformed and cross-cut all other structures. Further exhumation of the lower crustal rocks was not accompanied by tectonic events. All deformation fabrics were thoroughly annealed during subsequent slow cooling." @default.
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- W2027681330 date "1994-02-01" @default.
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- W2027681330 title "Large-scale thrusting in the lower crustal basement of Sri Lanka" @default.
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