Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari

River Widoro at UTM coordinate 04500601912798Z as a location of transition zone Sambipitu-Oyo Formation, consist of sandy limestone, covered by terrace deposits. Profile research of sandy limestone saprolite based on outcrop and thin section. Bed rock is sandy allochem limestone (Hu-1), has a lamina...

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Main Author: Perpustakaan UGM, i-lib
Format: Article
Published: [Yogyakarta] : Program Studi S1 Gizi Kesehatan Fak. Kedokteran UGM 2006
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author Perpustakaan UGM, i-lib
author_facet Perpustakaan UGM, i-lib
author_sort Perpustakaan UGM, i-lib
collection UGM
description River Widoro at UTM coordinate 04500601912798Z as a location of transition zone Sambipitu-Oyo Formation, consist of sandy limestone, covered by terrace deposits. Profile research of sandy limestone saprolite based on outcrop and thin section. Bed rock is sandy allochem limestone (Hu-1), has a lamination structure, experience corrosion and oxidation. The lower saprolite horizon is muddy allochem limestone (Hu-2), fractured with sharp boundary, develop tepee and relict of lamination structure. Continously water reaction from terrace deposits to rock produce mineral addition, dissolved and chemical weathering. Allochemic mudstone (Hu-3) is the upper saprolite horizon with relict texture of bed rock. Ore mineral, clay, and ferro oxide in Hu-3 are increase, sparite dissolved. Structural and textural changes as a result of water volume and turbidity are still strong.
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spelling oai:generic.eprints.org:206282014-06-18T00:25:40Z https://repository.ugm.ac.id/20628/ Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari Perpustakaan UGM, i-lib Jurnal i-lib UGM River Widoro at UTM coordinate 04500601912798Z as a location of transition zone Sambipitu-Oyo Formation, consist of sandy limestone, covered by terrace deposits. Profile research of sandy limestone saprolite based on outcrop and thin section. Bed rock is sandy allochem limestone (Hu-1), has a lamination structure, experience corrosion and oxidation. The lower saprolite horizon is muddy allochem limestone (Hu-2), fractured with sharp boundary, develop tepee and relict of lamination structure. Continously water reaction from terrace deposits to rock produce mineral addition, dissolved and chemical weathering. Allochemic mudstone (Hu-3) is the upper saprolite horizon with relict texture of bed rock. Ore mineral, clay, and ferro oxide in Hu-3 are increase, sparite dissolved. Structural and textural changes as a result of water volume and turbidity are still strong. [Yogyakarta] : Program Studi S1 Gizi Kesehatan Fak. Kedokteran UGM 2006 Article NonPeerReviewed Perpustakaan UGM, i-lib (2006) Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari. Jurnal i-lib UGM. http://i-lib.ugm.ac.id/jurnal/download.php?dataId=3481
spellingShingle Jurnal i-lib UGM
Perpustakaan UGM, i-lib
Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari
title Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari
title_full Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari
title_fullStr Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari
title_full_unstemmed Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari
title_short Endapan Teras Sebagai Kendali Profil Saprolit Kasus Zone Transisi Formasi Sambipitu-Oyo di Sungai Widoro Km.28,10 Yogyakarta-Wonosari
title_sort endapan teras sebagai kendali profil saprolit kasus zone transisi formasi sambipitu oyo di sungai widoro km 28 10 yogyakarta wonosari
topic Jurnal i-lib UGM
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