Greywackes with a Primary Matrix from the Viqueque Formation (Upper Miocene-Pliocene), Timor
1967; Society for Sedimentary Geology; Volume: Vol. 37; Linguagem: Inglês
10.1306/74d7163b-2b21-11d7-8648000102c1865d
ISSN1938-3681
Autores Tópico(s)earthquake and tectonic studies
ResumoABSTRACT The silt-clay matrix of the greywackes in the Viqueque Formation of Timor is considered to be an original detrital deposit and not the result of post-depositional diagenesis of sand grains. These late-Tertiary greywackes from Timor are associated with calcilutites and calcarenites. This association and the origin of these greywackes are related to their oceanic and tectonic milieu.
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