Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia
The study focused on the geology and provenance of the sandstone within Sambipitu Formation of Nglipar area. Petrography analysis were made on eight samples along the Kedungkeris River and paleocurrent analysis were made at Sungai Ngalang of Sambipitu Formation. Study area is comprised of five units...
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2018
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my.umk.eprints.50682022-05-23T08:38:18Z http://discol.umk.edu.my/id/eprint/5068/ Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia Nabilah Mohd Khair The study focused on the geology and provenance of the sandstone within Sambipitu Formation of Nglipar area. Petrography analysis were made on eight samples along the Kedungkeris River and paleocurrent analysis were made at Sungai Ngalang of Sambipitu Formation. Study area is comprised of five units if lithology which is tuffaceous sandstone, volcanic breccia unit, sandstone unit, carbonate sandstone unit and limestone unit that ranging from early Miocene to Late Miocene. Petrographic analysis shows that the sources of the sediment in study area are recycled orogen. In addition, the paleocurrent analysis also show that the direction of flow of the sediment is in NW-SE direction. 2018 Undergraduate Final Project Report NonPeerReviewed Nabilah Mohd Khair (2018) Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia. Final Year Project thesis, Universiti Malaysia Kelantan. (Submitted) |
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The study focused on the geology and provenance of the sandstone within Sambipitu Formation of Nglipar area. Petrography analysis were made on eight samples along the Kedungkeris River and paleocurrent analysis were made at Sungai Ngalang of Sambipitu Formation. Study area is comprised of five units if lithology which is tuffaceous sandstone, volcanic breccia unit, sandstone unit, carbonate sandstone unit and limestone unit that ranging from early Miocene to Late Miocene. Petrographic analysis shows that the sources of the sediment in study area are recycled orogen. In addition, the paleocurrent analysis also show that the direction of flow of the sediment is in NW-SE direction. |
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Undergraduate Final Project Report |
author |
Nabilah Mohd Khair |
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Nabilah Mohd Khair Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia |
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Nabilah Mohd Khair |
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Nabilah Mohd Khair |
title |
Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia |
title_short |
Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia |
title_full |
Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia |
title_fullStr |
Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia |
title_full_unstemmed |
Geology and sandstone provenance of the Sambipitu Formation in Nglipar area, Gunung Kidul regency, Yogyakarta special province, Indonesia |
title_sort |
geology and sandstone provenance of the sambipitu formation in nglipar area, gunung kidul regency, yogyakarta special province, indonesia |
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2018 |
url |
http://discol.umk.edu.my/id/eprint/5068/ |
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1763303501872496640 |
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13.211869 |