Depositional model of Ngrayong Formation in Madura Area, North East Java Basin, Indonesia

Paike Htwe, Sapto Surjono Surjono, Donatus Hendra Amijaya, Kyuro Sasaki

Research output: Contribution to journalArticle

Abstract

The early Middle Miocene Ngrayong Formation, an important reservoir of North East Java Basin, is well exposed in the central anticlinal part of Madura Island. The purpose of current study is to classify the epositional environments of the study area based on the characteristics and geometry of sedimentary facies. In the Madura island, the thicker clastics and deeper carbonates of Ngimbang Formation and Kujung Formation of Late Oligocene-Early Miocene deposited in the northeast-southwest asymmetrical half grabens. After the deposition of Kujung Formation, the basin morphology developed nearly eastwest trending shelf edge and the deposition of Tuban Formation began. The fine grained complex of Tuban Formation was followed by the Ngrayong Sandstones deposition. The depositional model of Ngrayong Formation is being producing of wide variety of depositional environments. Large scale cross-bedded sandstones and bioturbated massive sandstones with thin to medium bedded argillaceous limestone that outcrop in the northern part of the study area are deposited in costal environment. The heterolithic sandstone with planar and trough cross-lamination, fine grained sandstone with interlaminated structure and bioclastic carbonate exposed in the central part of the study area are deposited in upper shallow marine area. Dark grey siltstones and mudstones deposited in lower shallow marine area are well exposed in southern part of the study area. In conclusion, Ngrayong Formation in Madura area is developed in three depositional units which are coastal, upper shallow marine and lower shallow marine.
Original languageEnglish
Pages (from-to)49-58
Number of pages10
JournalJournal of Applied Geology
Volume7
Issue number2
Publication statusPublished - Dec 2015

Fingerprint

Sandstone
sandstone
basin
Carbonates
Miocene
carbonate
lamination
shelf break
Limestone
siltstone
depositional environment
mudstone
Oligocene
trough
outcrop
limestone
geometry
Geometry

All Science Journal Classification (ASJC) codes

  • Geotechnical Engineering and Engineering Geology

Cite this

Depositional model of Ngrayong Formation in Madura Area, North East Java Basin, Indonesia. / Htwe, Paike; Surjono, Sapto Surjono; Amijaya, Donatus Hendra; Sasaki, Kyuro.

In: Journal of Applied Geology, Vol. 7, No. 2, 12.2015, p. 49-58.

Research output: Contribution to journalArticle

Htwe, Paike ; Surjono, Sapto Surjono ; Amijaya, Donatus Hendra ; Sasaki, Kyuro. / Depositional model of Ngrayong Formation in Madura Area, North East Java Basin, Indonesia. In: Journal of Applied Geology. 2015 ; Vol. 7, No. 2. pp. 49-58.
@article{c51b61e1ab05460ca142d9e5451e6437,
title = "Depositional model of Ngrayong Formation in Madura Area, North East Java Basin, Indonesia",
abstract = "The early Middle Miocene Ngrayong Formation, an important reservoir of North East Java Basin, is well exposed in the central anticlinal part of Madura Island. The purpose of current study is to classify the epositional environments of the study area based on the characteristics and geometry of sedimentary facies. In the Madura island, the thicker clastics and deeper carbonates of Ngimbang Formation and Kujung Formation of Late Oligocene-Early Miocene deposited in the northeast-southwest asymmetrical half grabens. After the deposition of Kujung Formation, the basin morphology developed nearly eastwest trending shelf edge and the deposition of Tuban Formation began. The fine grained complex of Tuban Formation was followed by the Ngrayong Sandstones deposition. The depositional model of Ngrayong Formation is being producing of wide variety of depositional environments. Large scale cross-bedded sandstones and bioturbated massive sandstones with thin to medium bedded argillaceous limestone that outcrop in the northern part of the study area are deposited in costal environment. The heterolithic sandstone with planar and trough cross-lamination, fine grained sandstone with interlaminated structure and bioclastic carbonate exposed in the central part of the study area are deposited in upper shallow marine area. Dark grey siltstones and mudstones deposited in lower shallow marine area are well exposed in southern part of the study area. In conclusion, Ngrayong Formation in Madura area is developed in three depositional units which are coastal, upper shallow marine and lower shallow marine.",
author = "Paike Htwe and Surjono, {Sapto Surjono} and Amijaya, {Donatus Hendra} and Kyuro Sasaki",
year = "2015",
month = "12",
language = "English",
volume = "7",
pages = "49--58",
journal = "Journal of Applied Geology",
issn = "2502-2822",
number = "2",

}

TY - JOUR

T1 - Depositional model of Ngrayong Formation in Madura Area, North East Java Basin, Indonesia

AU - Htwe, Paike

AU - Surjono, Sapto Surjono

AU - Amijaya, Donatus Hendra

AU - Sasaki, Kyuro

PY - 2015/12

Y1 - 2015/12

N2 - The early Middle Miocene Ngrayong Formation, an important reservoir of North East Java Basin, is well exposed in the central anticlinal part of Madura Island. The purpose of current study is to classify the epositional environments of the study area based on the characteristics and geometry of sedimentary facies. In the Madura island, the thicker clastics and deeper carbonates of Ngimbang Formation and Kujung Formation of Late Oligocene-Early Miocene deposited in the northeast-southwest asymmetrical half grabens. After the deposition of Kujung Formation, the basin morphology developed nearly eastwest trending shelf edge and the deposition of Tuban Formation began. The fine grained complex of Tuban Formation was followed by the Ngrayong Sandstones deposition. The depositional model of Ngrayong Formation is being producing of wide variety of depositional environments. Large scale cross-bedded sandstones and bioturbated massive sandstones with thin to medium bedded argillaceous limestone that outcrop in the northern part of the study area are deposited in costal environment. The heterolithic sandstone with planar and trough cross-lamination, fine grained sandstone with interlaminated structure and bioclastic carbonate exposed in the central part of the study area are deposited in upper shallow marine area. Dark grey siltstones and mudstones deposited in lower shallow marine area are well exposed in southern part of the study area. In conclusion, Ngrayong Formation in Madura area is developed in three depositional units which are coastal, upper shallow marine and lower shallow marine.

AB - The early Middle Miocene Ngrayong Formation, an important reservoir of North East Java Basin, is well exposed in the central anticlinal part of Madura Island. The purpose of current study is to classify the epositional environments of the study area based on the characteristics and geometry of sedimentary facies. In the Madura island, the thicker clastics and deeper carbonates of Ngimbang Formation and Kujung Formation of Late Oligocene-Early Miocene deposited in the northeast-southwest asymmetrical half grabens. After the deposition of Kujung Formation, the basin morphology developed nearly eastwest trending shelf edge and the deposition of Tuban Formation began. The fine grained complex of Tuban Formation was followed by the Ngrayong Sandstones deposition. The depositional model of Ngrayong Formation is being producing of wide variety of depositional environments. Large scale cross-bedded sandstones and bioturbated massive sandstones with thin to medium bedded argillaceous limestone that outcrop in the northern part of the study area are deposited in costal environment. The heterolithic sandstone with planar and trough cross-lamination, fine grained sandstone with interlaminated structure and bioclastic carbonate exposed in the central part of the study area are deposited in upper shallow marine area. Dark grey siltstones and mudstones deposited in lower shallow marine area are well exposed in southern part of the study area. In conclusion, Ngrayong Formation in Madura area is developed in three depositional units which are coastal, upper shallow marine and lower shallow marine.

UR - https://jurnal.ugm.ac.id/jag/article/view/16934

M3 - Article

VL - 7

SP - 49

EP - 58

JO - Journal of Applied Geology

JF - Journal of Applied Geology

SN - 2502-2822

IS - 2

ER -