TY - JOUR
T1 - Sandstone diagenesis interpretation of Cipacar formation based on outcrop data in Banjarsari District, Lebak Regency, Banten
AU - Mahesa, F. G.
AU - Riyanto, A.
AU - Indraswari, A. O.
N1 - Funding Information:
This work was financially supported by Universitas Indonesia under research grant PIT 9 with grant contract number NKB-0033/UN2.R3.1/HKP.05.00/2019.
Publisher Copyright:
© 2021 Journal of Physics: Conference Series.
Copyright:
Copyright 2021 Elsevier B.V., All rights reserved.
PY - 2021/1/12
Y1 - 2021/1/12
N2 - The diagenesis of sediments is profoundly impacted by porosity and permeability since these parameters control the flow of fluids through rocks that build up mineral authigenesis, cementation, and dissolution. Porosity in rock is available in sedimentary rock, particularly in sandstone in Cipacar formation located in Banjarsari, Lebak, Banten. This research aims to examine sandstone characteristics, porosity value, diagenesis process, and implication between porosity and diagenesis. The data of this study were obtained from surface outcrops and petrographic analysis. Results of this research show that sandstones in Cipacar formation have porosity values between 8-14 % and have undergone diagenesis processes such as compaction, cementation, and dissolution which are classified in the mesogenesis regime.
AB - The diagenesis of sediments is profoundly impacted by porosity and permeability since these parameters control the flow of fluids through rocks that build up mineral authigenesis, cementation, and dissolution. Porosity in rock is available in sedimentary rock, particularly in sandstone in Cipacar formation located in Banjarsari, Lebak, Banten. This research aims to examine sandstone characteristics, porosity value, diagenesis process, and implication between porosity and diagenesis. The data of this study were obtained from surface outcrops and petrographic analysis. Results of this research show that sandstones in Cipacar formation have porosity values between 8-14 % and have undergone diagenesis processes such as compaction, cementation, and dissolution which are classified in the mesogenesis regime.
KW - Cipacar formation
KW - Diagenesis
KW - Porosity
KW - Sandstone
UR - http://www.scopus.com/inward/record.url?scp=85100703365&partnerID=8YFLogxK
U2 - 10.1088/1742-6596/1725/1/012079
DO - 10.1088/1742-6596/1725/1/012079
M3 - Conference article
AN - SCOPUS:85100703365
SN - 1742-6588
VL - 1725
JO - Journal of Physics: Conference Series
JF - Journal of Physics: Conference Series
IS - 1
M1 - 012079
T2 - 2nd Basic and Applied Sciences Interdisciplinary Conference 2018, BASIC 2018
Y2 - 3 August 2018 through 4 August 2018
ER -