Jurnal Sains dan Teknologi
Vol. 5 No. 1 (2026): Februari 2026

Characteristics of the Viqueque Formation in the Caraubalo Area, Viqueque District, Timor-Leste

M. Faustino (Unknown)
P. Setyo (Unknown)
Astuti B. S. (Unknown)



Article Info

Publish Date
10 Feb 2026

Abstract

This research was conducted in the Cuha River, within the Buanurak area of Caraubalo Village, Viqueque District, Timor-Leste. The study area is geographically located between 08⁰49’29”S - 08⁰52'28”S and 126⁰23'8”E - 126⁰20'8”E. The objective was to characterize the facies of the Viqueque Formation through field data. The methodology involved measuring a stratigraphic cross-section, with subsequent analysis based on the parameters of the Bouma (1962), Walker (1979), and Mutti concepts. Analysis identified four main lithological units. Facies A1-A3 consist of gray marl, deposited by low-density turbidity currents in a lower fan setting (Td-Te Bouma intervals; F9a Fine Grain Facies). Facies B1-B2 feature interbedded sandstone and marl with parallel lamination, representing deposition in suprafan lobes (CT-2 sequence; F7 Fine Grain Facies). Facies C is characterized by normally graded conglomerates, interpreted as mid-fan channel deposits. Finally, Facies D comprises polymict conglomerates, deposited by high-density turbidity currents in an upper fan setting, corresponding to the CGL-7 facies (F9b) and the Ta Bouma interval.

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