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Based on regional fisiography in Easterm part of Central Java, research area is located in Kendeng Zone and Solo Zone. Study area is divided into 2 geomorphology units which are Ridge Homoklin and Aluvial Plains. Stratigraphy unit in study area divided into 4 unofficial lithology unit from oldest to...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/13910 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Based on regional fisiography in Easterm part of Central Java, research area is located in Kendeng Zone and Solo Zone. Study area is divided into 2 geomorphology units which are Ridge Homoklin and Aluvial Plains. Stratigraphy unit in study area divided into 4 unofficial lithology unit from oldest to youngest lithology units. Marl-Limestone Unit which was deposited in Late Miocene and then Marl-Sandstone was deposited above it in early Pliocene, Limestone unit was deposited in Pliocene and wedges with Marl-Sandstone unit. In Post Pliocene, tectonic activity occured and caused layer has dip, fault and uplift, then erosion occured and caused geomorphology forming. In Recent, Aluvial Unit was deposited. Structure geology which appears in study area is intrepretation strike-slip fault that is Strike Slip Fault Tangen, Strike Slip Fault Katelan and Strike Slip Fault Dunggringan. |
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