REGIONAL GEOLOGY OF KEREK, NGAWI, EAST JAVA PROVINCE

Jun 30th, 2015
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This research is located in Kerek, Kabupaten Ngawi, East Java. This area is located in 7° 22' 00" LS - 7°24' 30" LS & 111° 27' 30" BT - 111° 29' 30" BT and this area is about 17 km2 wide. The purpose of this research is to make the geological map and determine the geomorphological units, stratigraphy units, geological structure, and geological history of Kerek. The method of this research is study of the literature, field observation, and laboratory experiment.

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REGIONAL GEOLOGY OF KEREK, NGAWI, EAST JAVA PROVINCERyan Damara Pradhana , Yan Rizal , FadhelDepartment of Geological EngineeringFaculty of Earth Science and TechnologyInstitute of Technology BandungAbstractThis research is located in Kerek, Kabupaten Ngawi, East Java. This area is located in 7 22' 00" LS - 724' 30" LS & 111 27' 30" BT - 111 29' 30" BT and this area is about 17 km2 wide. The purpose of this research is to make the geological map and determine the geomorphological units, stratigraphy units, geological structure, and geological history of Kerek. The method of this research is study of the literature, field observation, and laboratory experiment. Geomorphology of research area is divided into fold hills unit, homoclinal hills unit, and railroad river unit. Stratigraphy of research area is divided into 8 units, that is sandstone-tuff unit that deposited on Late Miocene, tuff I unit that deposited on Early Pliocene, marl unit that deposited on Early Pliocene, limestone unit that deposited on Early Pliocene, tuff II unit that deposited on Early Pliocene, breccia unit that deposited on Late Pliocene, railroad river unit that deposited on Holocene, and alluvial unit that deposited on Holocene. Geological structure that developed in this area is Kerek reverse fault trending northeast-southwest and Banyuurip transform fault trending north-south.Keywords: Kerek, Ngawi, Stratigraphy, GeolomorphologyINTRODUCTIONKerek is a village located in Ngawi, E

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