Lapangan Gunung Api Tersier Daerah Berbah Sleman - Imogiri Bantul,Yogyakarta
<p>In the area of Berbah - Sleman to Imogiri - Bantul Districts, Yogyakarta Tertiary volcanic rocksform a hummocky topography. Those volcanic rocks comprise coherent lavas and volcaniclastic rocks having basalt to basaltic andesite in composition. Genetically, the rocks are pillow lavaflows,...
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| 格式: | Article NonPeerReviewed |
| 出版: |
[Yogyakarta] : Departemnts of Geological Engineering Faculty of E
2009
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| 在線閱讀: | https://repository.ugm.ac.id/95185/ http://repository.ugm.ac.id/digitasi/index.php?module=cari_hasil_full&idbuku=3003 |
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| 機構: | Universitas Gadjah Mada |
| 總結: | <p>In the area of Berbah - Sleman to Imogiri - Bantul Districts, Yogyakarta Tertiary volcanic rocksform a hummocky topography. Those volcanic rocks comprise coherent lavas and volcaniclastic rocks having basalt to basaltic andesite in composition. Genetically, the rocks are pillow lavaflows, dikes. pyroclastics and resedimented (syn-eruptive) deposits. Previous workers stated that the hummocky topography was controlled by tectonic faulting. Based on volcanic geology study it is believed that the landscape is a volcanic field consisting some paleo volcanic cones. The volcanic field is distributed in NE-SW direction. Perhaps, this pattern was controlled by a subsurface fault. and then reactivated to cut the volcanic cones. Volcanic activities in this area varied from monogenetic cones, such as Watuadeg paleovolcano, developing to the Sudimoro composite volcano.</p> |
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