Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara

Authors

  • David Victor Mamengko Fakultas Teknik Geologi Universitas Padjadjaran
  • Yoga B.Sendjadja Universitas Padjadjaran
  • Budi Mulyana Universitas Padjadjaran
  • Hermes Panggabean Pusat Survei Geologi
  • Iyan Haryanto Universitas Padjadjaran
  • Eko Budi Lelono
  • Juwita Trivianty Musu Lemigas
  • Panuju Panuju Lemigas

DOI:

https://doi.org/10.33332/jgsm.geologi.v20i1.399

Abstract

North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result  shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.

Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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Published

2019-02-25

Issue

Vol. 20 No. 1 (2019): Jurnal Geologi dan Sumberdaya Mineral

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