IDENTIFIKASI KESTABILAN LERENG MENGGUNAKAN NORMALIZED DIFFERENCE VEGETATION I…

The location of this study is in the Sukamaju area, Bogor regency, West Java province. The research location is located in Mandala Basin Bogor. Mandala Bogor Basin according to Martodjojo (1984) ha…

ANALISIS PENGARUH INTENSITAS CURAH HUJAN TERHADAP KESTABILAN LERENG BERDASARK…

Tanah longsor merupakan salah satu bencana alam geologi berupa terjadinya gerakan tanah atau massa batuan penyusun lereng yang sewaktu-waktu dapat menimbulkan kerugian materil bahkan korban jiwa. T…

ANALISIS MORFOTEKTONIK DAN CURAH HUJAN SERTA IMPLIKASINYA TERHADAP LONGSOR PA…

Secara geografis daerah penelitian terletak di Desa Gunung Megang, Kecamatan Semidang Alas, Kabupaten Seluma, Bengkulu. Penelitian bertujuan untuk mengetahui aktivitas tektonik dan tingkat curah hu…

ANALISIS MORFOMETRI TERHADAP PERUBAHAN ALUR SUNGAI KALI BEKASI BERBASIS SISTE…

Kali Bekasi River is located in Bogor Regency, West Java Province which is geologically included in the Bogor Regional Geological Map. The research area is 9x9 km which passes through 2 formations,…

EVOLUSI TEKTONIK BATUAN DASAR BUKIT GARBA SUMATERA SELATAN

Edition

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ISBN/ISSN

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Collation

xxiii, 174 hlm.; ilus.; 29 cm

Series Title

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Call Number

T893202023

ANALISIS KERAWANAN LONGSOR DENGAN MENGGUNAKAN METODE ANALYTICAL HIERARCHY PRO…

This geological assessment is carried out to identify the potential hazards of landslides in the surrounding area and efforts to overcome them. This research is focused on Keban Agung and its surro…

 ANALISIS MORFOTEKTONIK DAN IMPLIKASINYA TERHADAP LONGSOR DAERAH TANJUNG AGU…

The research is located in the Tanjung Agung area, including the Sumatra Selatan Basin, with active tectonic conditions. Research at this location is intended to identify the level of tectonic acti…

STUDI STRATIGRAFI PADA FORMASI TALANG AKAR BERDASARKAN DATA PERMUKAAN DAERAH …

The Sukomoro area and its surroundings, Banyuasin Regency, South Sumatera have characteristics of sedimentary rocks of late Oligocene to Early Miocene age which were deposited in the South Sumatera…

IDENTIFIKASI PALEOEKOLOGI FORMASI MENGKARANG LINTASAN SUNGAI BATANG MERANGIN …

Sungai Batang Merangin berada di Kabupaten Merangin, Provinsi Jambi. Sungai Batang Merangin merupakan bagian dari Formasi Mengkarang. Metode penelitian yang dilakukan untuk mengidentifikasi aspek g…

ANALISIS POTENSI AIR BERSIH DAERAH MUARA BULIAN, KABUPATEN BATANG HARI, PROVI…

Groundwater can be defined as all the air contained in the basic space or regolith (Aziz, 2000). This research is located in Muara Bulian Subdistrict and its surroundings in Batanghari Regency, Jam…

ANALISIS MORFOTEKTONIK DAN IMPLIKASINYA TERHADAP LONGSOR DAERAH TANJUNG SAKTI…

Lokasi penelitian terletak di Desa Tanjung Sakti, Kecamatan Tanjung Sakti Pumi, Kabupaten Lahat, Sumatera Selatan. Daerah ini termasuk ke dalam Cekungan Bengkulu dengan kondisi tektonik yang masih …

ANALISIS MIKROFASIES BATUGAMPING FORMASI BATURAJA DAERAH PUSAR DAN SEKITARNYA…

Lokasi penelitian batugamping berada di Daerah Pusar, Kabupaten Ogan Komering Ulu, Provinsi Sumatera Selatan. Batugamping Formasi Baturaja mempunyai karakteristik litologi yang menarik untuk dilaku…

STUDI PROVENANCE BATUPASIR FORMASI GUMAI DAERAH TALANG MERBAU DAN SEKITARNYA,…

The research location is in the village of Talang Merbau and its surroundings, South OKU Regency, South Sumatra which aims to study the provenance of the sandstones of the Gumai Formation by conduc…

 IDENTIFIKASI ALTERASI HIDROTERMAL PADA BATUAN VULKANIK FORMASI JAMPANG DI D…

Proses alterasi hidrotermal terjadi akibat adanya interaksi antara fluida hidrotermal terhadap batuan yang dilaluinya atau yang dikenal dengan istilah wall rocks. Akibat dari proses interaksi terse…

 IDENTIFIKASI KERAWANAN LONGSOR PADA JALAN LINTAS PROVINSI KECAMATAN TANJUNG…

This research is located in the administrative area District of Tanjung Sakti Pasemah Ulu Manna Ilir (PUMI), Lahat Regency, South Sumatra. Geologically, it is located in the barisan mountains (volc…

ANALISIS KESTABILAN LERENG MENGGUNAKAN METODE SIMPLIFIED BISHOP PADA DAERAH P…

The research locations are in Pulau Pinang District and its surroundings, Lahat Regency. Geographically the study area is located at 48 M 332724.86 E and 48 M 9575483.42 S. The purpose of this rese…

ANALISIS PERUBAHAN MORFOLOGI SUNGAI KEDURANG SEBAGAI RESPON TERHADAP STRUKTUR…

The Kedurang River is a river located in Batuampar Village, Kedurang District, South Bengkulu Regency, Bengkulu Province. The headwaters of the Kedurang river are in the Rajamandara Mountains and d…

ANALISA GEMPA BUMI MENGGUNAKAN ANALISIS MORFOTEKTONIK DAERAH MUBA DAN SEKITAR…

The research was conducted in Muba and its surroundings, South Sumatra. This area is included in the back arc basin which is not uncommon for geological disasters, one of which is an earthquake. Th…

ANALISIS MORFOMETRI TERHADAP PERUBAHAN SUNGAI MENGGUNAKAN PENGINDERAAN JAUH P…

Batang Sukam river is located in Sijunjung Regency, West Sumatra with a research area of 9 x 9 km. The changes that occur are caused by several factors such as erosion processes and deposition, the…

STUDI DIAGENESIS BATUGAMPING ANGGOTA MERSIP FORMASI PENETA BERDASARKAN ANALIS…

The existence of limestone lithology in the Jambi Sub-Basin is an interesting phenomenon to study on the type, environment and stages of the limestone diagenesis process. The research is devoted to…

ANALISIS MORFOMETRI SUNGAI DAN PERUBAHAN FUNGSI LAHAN PADA SUB DAERAH ALIRAN …

Administratively, the Way Tebu River is located in Pugung District, Tanggamus Regency, Lampung with a study area of 9 x 9 km. This study aims to analyze changes in meander morphometric parameters a…

PENENTUAN IKLIM PURBA BERDASARKAN FORAMINIFERA PADA FORMASI GUMAI DAERAH KUNG…

Kungkilan is located in Ogan Komering Ulu Regency, South Sumatra Province, which is 35 minutes drive from Baturaja City. This study aims to determine how the ancient climate conditions in the Gumai…

PETROGENESA BATUAN VULKANIK FORMASI JAMPANG DAERAH CIKUPA DAN SEITARNYA, KABU…

Penelitian mengenai petrogenesis batuan vulkanik penyusun Formasi jampang (Tomj) dilakukan di Daerah Cikupa, Kabupaten Ciamis, Provinsi Jawa Barat. Penelitian ini bertujuan untuk memahami karakteri…

ENDAPAN TURBIDIT FORMASI HALANG DAERAH BERTA DAN SEKITARNYA, BANJARNEGARA, JA…

Daerah penelitian berada di Desa Berta dan sekitarnya, Kecamatan Susukan, Kabupaten Banjarnegara, Jawa Tengah. Luasan daerah penelitian 3x3,5 Km memiliki karakteristik penciri endapan turbidit Form…

STUDI MIKROFASIES BATUGAMPING FORMASI KALIPUCANG, DAERAH URUG DAN SEKITARNYA,…

Penelitian mengenai mikrofasies batugamping Formasi Kalipucang dilakukan di daerah Urug dan sekitarnya, Kecamatan Jatiwaras, Kabupaten Tasikmalaya, Jawa Barat. Formasi Kalipucang merupakan kelompok…

ANALISIS MORFOTEKTONIK DAN IMPLIKASINYA TERHADAP LONGSOR DAERAH BRUNO KABUPAT…

Secara geografis daerah penelitian terletak di Kecamatan Bruno, Kabupaten Purworejo, Jawa Tengah. Daerah ini termasuk ke dalam Zona Serayu Selatan, dimana aktivitas tektonik pada zona ini berlangsu…

ANALISIS MORFOLOGI TERHADAP POTENSI PEMBANGKIT LISTRIK TENAGA MIKROHIDRO DAER…

ABSTRAK Penelitian analisis morfologi terhadap potensi pembangkit listrik tenaga mikrohidro dilakukan pada pada hulu sungai Batang Anai daerah Singgalang dan sekitarnya Kabupaten Tanah Datar, Sumat…

ANALISIS MORFOMETRI TERHADAP PERUBAHAN ALUR SUNGAI PULASAN, KABUPATEN SIJUNJU…

Pulasan River is located in Sijunjung District, Sijunjung Regency, West Sumatra Province. Geologically included in the Solok Map sheet, the research was did in an area of 9 x 9 km which contains se…

HILIRISASI LIMBAH HASIL PENGOLAHAN ANDESIT SEBAGAI BAHAN CAMPURAN PEMBUATAN B…

Developments in the industrial sector that not only have posistif implications but also have negative implications, such as industrial waste that accumulates every day therefore must be utilized. U…

ANALISIS KERAWANAN LONGSOR MENGGUNAKAN INDEX PROPERTIES TANAH DALAM MITIGASI …

The research location is in the Puspahiang area, Tasikmal aya Regency, West Java, where most of the Tasikmalaya area consists of moderate plains with an altitude of 250 to 750 meters, and the level…