local_ids_str_mv IOS1.17136
IOS69.article-8278
ctrlnum 17136
article-8278
language eng
ind
format Journal:Article
Journal
PeerReview:NonPeerReviewed
PeerReview
Book:Book
Book
author Faizal Muhamadsyah,
Edy Sunardi,
Vijaya Isnaniawardhani,
-, Faizal Muhamadsyah
-, Edy Sunardi
-, Vijaya Isnaniawardhani
title Karakteristik Geologi Daerah Gunungan Lumpur Ciuyah
publishDate 2012
topic Abstrak
mud flows
morphometry
geological structure
url http://repository.unpad.ac.id/17136/1/pustaka_unpad_karakteristik_geologi_daerah_gunungan.pdf
http://repository.unpad.ac.id/17136/
http://jurnal.unpad.ac.id/bsc/article/view/8278
http://jurnal.unpad.ac.id/bsc/article/view/8278/3825
contents Gunungan lumpur yang teridentifikasi di daerah Ciuyah terletak di Desa Ciniru, Kecamatan Ciniru, Kabupaten Kuningan, Jawa Barat. Kajian morpometri melalui penyebaran kelas lereng telah menggambarkan distribusi kelas secara konsentris dengan lokasi gunungan Ciuyah di bagian tengah. Pola aliran sungai annular dalam skala regional menunjukan gambaran sirkular di daerah Ciniru disekitar lokasi ekstrusi gunungan lumpur Ciuyah. Pola-pola sirkular yang diperlihatkan oleh distribusi zona kemiringan lereng dan pola aliran sungai yang annular dalam skala yang lebih regional menyugestikan adanya updoming di bawah permukaan. Ditafsirkan bahwa jalur-jalur migrasi dan kemungkinan sirkulasi fluida dikontrol oleh patahan-patahan yang berkembang di daerah penelitian. Struktur geologi merupakan faktor-faktor yang mendukung terjadinya pelepasan atau migrasi fluida ke permukaan dan memberikan jalan keluar bagi materi-materi dan fluida yang berada di bawah kondisi tekanan yang berlebih, material lempungan yang menyusun formasi batuan dasar mengalami proses elusiasi, dan akhirnya membentuk intruksi gunungan lumpur di permukaan. The mud flow which indentified in Ciuyah area localed in Ciniru, Kecamatan Ciniru Kuningan regency, West Java. Study of morphometry through the development of slope classes have described the class as a concentric with location of Ciuyah mud flow in the middle. Annular's drainage pattern as the regional scale is reflected of the circular in the Ciniru area, at around of site extrusion Ciuyah mud mound. Circular patterns of distribution shown by the scale zone, and annular flow patterns in the river a more regional scale is suggest updoming beneath the surface. Interpreted that the migration channel and the possible fluid circulation is controlled by faults that developed in the study area. Structural geology are factors that contribute to the release or migration of fluid to the surface, and provide an outlet for material and fluid under conditions of excessive stress, clayey material which forming of bedrock formations is elusiation experience process, and eventually formed mountains of mud intrusion on the surface.
The mud flow which identified in Ciuyah area is located in Ciniru village, District Ciniru, Kuningan regency, West Java. Study of morphometry through the deployment of slope classes have described the class as a concentric distribution with location of Ciuyah mud flow in the middle. Annular’s drainage pattern at the regional scale is reflected of the circular in the Ciniru area, at around of site Ciniru extrusion Ciuyah mud mound. Circular patterns of distribution shown by the slope zone, and annular flow patterns in the river a more regional scale is suggest updoming beneath the surface. Interpreted that the migration channel and the possible fluid circulation is controlled by faults that developed in the study area. Structural geology are factors that contribute to the release or migration of fluid to the surface, and provide an outlet for material and fluid under conditions of excessive stress, clayey material which forming of bedrock formations is elusiation experience process, and eventually formed mountains of mud intrusion on the surface
institution Universitas Padjadjaran
collection Repositori UNPAD
Bulletin of Scientific Contribution
first_indexed 2016-11-06T05:22:42Z
author2 Fakultas Teknik Geologi
publisher fakultas Teknik Geologi Universitas Padjadjaran
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