The research area is located in the Nagari Airangat area, Sijunjung District, Sijunjung Regency, West Sumatra. The study area is at coordinates 0 ° 35 '41.6436 "- 0 ° 36' 46.3932" South Latitude and 100 ° 54 '58.1724 "- 100 ° 56' 35.3076" East longitude. The purpose of this study was to determine the process of diagenesis that works on limestone in the study area, determine the environmental conditions of limestone diagenesis in the study area, determine the stages and models of diagenesis that work on limestone in the study area. The method used in this study is by petrographic incision. The study area limestone is included in the formation of Kuantan and research results from 9 samples, there are 4 types of mudstone limestone, limestone l...
The geological mapping is carried out at Panggung lalat which is a part of district of Gua Musang, K...
The sedimentary rock is formed and associated with the diagenesis processes, as all the physical, ch...
The large scale of geological map (1: 750 000) does not give sufficient information about each outcr...
Geographycally the research area lies between 00 43′ 38′′ – 00 40′ 56′′ North Latitude and 1010 29′ ...
Fomasi Kuantan merupakan batuan tertua pada terrane Sumatra Barat yang tersingkap di Ngalau Basurek,...
Proses pembentukan batugamping ditentukan oleh proses geologi yaitu sedimentasi, morfologi bawah per...
Proses pembentukan batugamping ditentukan oleh proses geologi yaitu sedimentasi, morfologi bawah per...
Penyebaran batugamping secara geologi yang berada di bagian tengah Cekungan Limboto menjadi daya tar...
Setul Formation is the oldest limestone dated from Ordovician to Silurian in Langkawi. It shows vari...
This study aims to determine the limestone facies and diagenesis on Tondo Formation. The method used...
Geographically, the study area is at 9241000 mN - mE 9235000 mN and 548 000 - 555 000 mE (UTM WGS 84...
Keberadaan litologi batuan karbonat berupa batugamping merupakan suatu fenomena yang khas dan menar...
Daerah penelitian terletak di Daerah Guluk-Guluk dan Sekitarnya Kabupaten Sumenep Provinsi Jawa Timu...
The study area is located at the southeast part of Gua Musang that bounded by longitude E 102̊ 04 18...
DOI: 10.17014/ijog.v7i2.138Limestone diagenetic records of Sentolo Formation have been studied in or...
The geological mapping is carried out at Panggung lalat which is a part of district of Gua Musang, K...
The sedimentary rock is formed and associated with the diagenesis processes, as all the physical, ch...
The large scale of geological map (1: 750 000) does not give sufficient information about each outcr...
Geographycally the research area lies between 00 43′ 38′′ – 00 40′ 56′′ North Latitude and 1010 29′ ...
Fomasi Kuantan merupakan batuan tertua pada terrane Sumatra Barat yang tersingkap di Ngalau Basurek,...
Proses pembentukan batugamping ditentukan oleh proses geologi yaitu sedimentasi, morfologi bawah per...
Proses pembentukan batugamping ditentukan oleh proses geologi yaitu sedimentasi, morfologi bawah per...
Penyebaran batugamping secara geologi yang berada di bagian tengah Cekungan Limboto menjadi daya tar...
Setul Formation is the oldest limestone dated from Ordovician to Silurian in Langkawi. It shows vari...
This study aims to determine the limestone facies and diagenesis on Tondo Formation. The method used...
Geographically, the study area is at 9241000 mN - mE 9235000 mN and 548 000 - 555 000 mE (UTM WGS 84...
Keberadaan litologi batuan karbonat berupa batugamping merupakan suatu fenomena yang khas dan menar...
Daerah penelitian terletak di Daerah Guluk-Guluk dan Sekitarnya Kabupaten Sumenep Provinsi Jawa Timu...
The study area is located at the southeast part of Gua Musang that bounded by longitude E 102̊ 04 18...
DOI: 10.17014/ijog.v7i2.138Limestone diagenetic records of Sentolo Formation have been studied in or...
The geological mapping is carried out at Panggung lalat which is a part of district of Gua Musang, K...
The sedimentary rock is formed and associated with the diagenesis processes, as all the physical, ch...
The large scale of geological map (1: 750 000) does not give sufficient information about each outcr...