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- W3196380587 abstract "Sri Lanka is a Gondwana fragment and consists of three distinct Proterozoic lithotectonic units, namely the Wanni Complex to the west, the centrally located Highland Complex, and the Vijayan Complex in the east. The boundaries between these lithotectonic units are major ductile shear zones. The three crustal units were amalgamated at two different stages during the formation of Gondwana. In this chapter, 87 key photographs from the three crustal units and their boundary shear zones are presented, which illustrate Proterozoic sedimentation and magmatism, high temperature deformation, amphibolite-granulite facies metamorphism, migmatization, shearing under high-grade conditions, partial melting, post-metamorphic metasomatism, and other late-stage crustal processes." @default.
- W3196380587 created "2021-09-13" @default.
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- W3196380587 date "2022-01-01" @default.
- W3196380587 modified "2023-09-25" @default.
- W3196380587 title "Proterozoic orogens of Sri Lanka" @default.
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- W3196380587 doi "https://doi.org/10.1016/b978-0-12-817978-9.00004-4" @default.
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