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ongoing orogenetic activities. Such activity may have been recorded in an accretionary orogen, that is, at Such activity may have been recorded in an accretionary orogen, that is, at the convergence and collision of an oceanic and a continental plate (Fyfe and Kerrich 1985).


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Malaga Sumatra orogene R. Do. - DWC

the rock formations of South Sumatra outside the Neogene basin of Djambi Palembang and the Lampoeng Districts are distributed over three main orogenetic units of major importance in the larger western half or Asiatic part of the East Indian Archipelago

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