Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan

<p><a href="http://dx.doi.org/10.17014/ijog.vol3no4.20081" target="_blank">http://dx.doi.org/10.17014/ijog.vol3no4.20081</a></p><p><em>Lithologically, the Nampurejo Pillow Lava, Kebo and Butak Formations, which are dominated by volcanic rocks,...

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Main Author: Surono Surono
Format: Article
Language:English
Published: Geological Agency 2014-06-01
Series:Indonesian Journal on Geoscience
Subjects:
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/59
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spelling doaj-2354ecef45e84f00818d88d7c18a6b9f2020-11-24T22:17:12ZengGeological AgencyIndonesian Journal on Geoscience2355-93142355-93062014-06-013418319310.17014/ijog.3.4.183-19359Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian SelatanSurono Surono0Pusat Survei Geologi, Badan Geologi, Jl. Diponegoro No. 57, Bandung<p><a href="http://dx.doi.org/10.17014/ijog.vol3no4.20081" target="_blank">http://dx.doi.org/10.17014/ijog.vol3no4.20081</a></p><p><em>Lithologically, the Nampurejo Pillow Lava, Kebo and Butak Formations, which are dominated by volcanic rocks, spread west - eastly, along the northern foot of the Baturagung Mountains. The Nampurejo Pillow Lava, which has an Early Oligocene age, is overlain by the Late Oligocene - Early Miocene Kebo and Butak Formations successively.</em></p> <p><em>The Nampurejo Pillow Lava consists of basaltic pillow-lavas showing pillow structures and they are intercalated by black sandstones. The Kebo Formation comprises alternating sandstone and pebbly sandstone with intercalations of siltstone, claystone, tuff, and shale. On the other hand, the Butak For- mation is composed of polymic breccia with intercalations of sandstone, pebbly sandstone, claystone, and siltstone/shale.</em></p> <p><em>The three units were deposited in a deep – shallow marine basin, which was filled by volcanic prod- ucts. Compared to the lower part of the Kebo Formation, volcanic activities during the deposition of the upper part of the Kebo Formation and the Butak Formation were more active.</em></p> <p> </p> <p> </p>https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/59Pillow lavaKeboButakvolcanodepositionBaturagung
collection DOAJ
language English
format Article
sources DOAJ
author Surono Surono
spellingShingle Surono Surono
Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan
Indonesian Journal on Geoscience
Pillow lava
Kebo
Butak
volcano
deposition
Baturagung
author_facet Surono Surono
author_sort Surono Surono
title Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan
title_short Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan
title_full Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan
title_fullStr Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan
title_full_unstemmed Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan
title_sort litostratigrafi dan sedimentasi formasi kebo dan formasi butak di pegunungan baturagung, jawa tengah bagian selatan
publisher Geological Agency
series Indonesian Journal on Geoscience
issn 2355-9314
2355-9306
publishDate 2014-06-01
description <p><a href="http://dx.doi.org/10.17014/ijog.vol3no4.20081" target="_blank">http://dx.doi.org/10.17014/ijog.vol3no4.20081</a></p><p><em>Lithologically, the Nampurejo Pillow Lava, Kebo and Butak Formations, which are dominated by volcanic rocks, spread west - eastly, along the northern foot of the Baturagung Mountains. The Nampurejo Pillow Lava, which has an Early Oligocene age, is overlain by the Late Oligocene - Early Miocene Kebo and Butak Formations successively.</em></p> <p><em>The Nampurejo Pillow Lava consists of basaltic pillow-lavas showing pillow structures and they are intercalated by black sandstones. The Kebo Formation comprises alternating sandstone and pebbly sandstone with intercalations of siltstone, claystone, tuff, and shale. On the other hand, the Butak For- mation is composed of polymic breccia with intercalations of sandstone, pebbly sandstone, claystone, and siltstone/shale.</em></p> <p><em>The three units were deposited in a deep – shallow marine basin, which was filled by volcanic prod- ucts. Compared to the lower part of the Kebo Formation, volcanic activities during the deposition of the upper part of the Kebo Formation and the Butak Formation were more active.</em></p> <p> </p> <p> </p>
topic Pillow lava
Kebo
Butak
volcano
deposition
Baturagung
url https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/59
work_keys_str_mv AT suronosurono litostratigrafidansedimentasiformasikebodanformasibutakdipegununganbaturagungjawatengahbagianselatan
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