TY - JOUR
T1 - The relationship of volcanic facies and temperature range derived from the associated clay mineral in Gunung Endut, Banten
AU - Primayudha, F.
AU - Sahdarani, D. N.
AU - Kadja, G. T.M.
AU - Supriyanto, null
N1 - Funding Information:
X-ray Diffraction and Petrography analyses on hydrothermal alteration Gunung Endut, Banten research is a part of Universitas Indonesia PITTA Grant 2018. Authors would also like to show it gratitude to Geoscience Study Program, Faculty of Mathematics and Natural Sciences, Universitas Indonesia and Study Program of Chemistry, Faculty of Mathematics and Natural Sciences, Institut Teknologi Bandung for supporting this research.
Publisher Copyright:
© 2021 Journal of Physics: Conference Series.
PY - 2021/1/12
Y1 - 2021/1/12
N2 - Gunung Endut located in Lebak, Banten is one of the prospected areas of geothermal energy resource on the island of Java, Indonesia. The presence of clay mineral in the surface can help to determine the hydrothermal fluid temperature circulating in Gunung Endut. Based on the collected samples, petrography analysis revealed the presence of clay minerals while diffraction method confirmed the presence of dickite, montmorillonite, kaolinite, pyrophyllite, chlorite, diaspore and illite. There are three different temperature range from each volcanic facies. It is predicted that clay minerals at their temperature range in Gunung Endut are formed based on the type of rocks and the topography of the research area.
AB - Gunung Endut located in Lebak, Banten is one of the prospected areas of geothermal energy resource on the island of Java, Indonesia. The presence of clay mineral in the surface can help to determine the hydrothermal fluid temperature circulating in Gunung Endut. Based on the collected samples, petrography analysis revealed the presence of clay minerals while diffraction method confirmed the presence of dickite, montmorillonite, kaolinite, pyrophyllite, chlorite, diaspore and illite. There are three different temperature range from each volcanic facies. It is predicted that clay minerals at their temperature range in Gunung Endut are formed based on the type of rocks and the topography of the research area.
KW - Clay mineral
KW - Gunung endut
KW - Petrography
KW - Volcanic facies
KW - XRD
UR - http://www.scopus.com/inward/record.url?scp=85100724326&partnerID=8YFLogxK
U2 - 10.1088/1742-6596/1725/1/012073
DO - 10.1088/1742-6596/1725/1/012073
M3 - Conference article
AN - SCOPUS:85100724326
SN - 1742-6588
VL - 1725
JO - Journal of Physics: Conference Series
JF - Journal of Physics: Conference Series
IS - 1
M1 - 012073
T2 - 2nd Basic and Applied Sciences Interdisciplinary Conference 2018, BASIC 2018
Y2 - 3 August 2018 through 4 August 2018
ER -