GEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA
Java is a familiar area to many interest of geology including oil and gas exploration. The Rembang-Madura-Kangean-Sakala (RMKS) area is one of the most common studied area in East Java. This research area covers Blora and Rembang district. Research area covering about 66 km2 is composed to six f...
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id-itb.:263632018-03-20T13:43:37ZGEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA Daniel Adipradipto, Geologi, hidrologi & meteorologi Indonesia Final Project North East Java Basin, RMKS, provenance, Ngrayong Formation, Ngiyono, Blora INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/26363 Java is a familiar area to many interest of geology including oil and gas exploration. The Rembang-Madura-Kangean-Sakala (RMKS) area is one of the most common studied area in East Java. This research area covers Blora and Rembang district. Research area covering about 66 km2 is composed to six formations, according to Peta Badan Geologi. Researcher found six litology units which can be differed descriptively in the field, they are Limestone I, Sandstone, Limestone II, Claystone, Limestone III, and Marl unit. These six units are Early Miocene to Holocene Age. The study area also has some geological structures, they are fold, strike-slip fault, normal fault, and faultbend fold. There is also a study of provenance of sandstone of Ngrayong Formation. Eight samples are classified as Recycled Orogen Provenance (Dickinson and Suczek, 1979). text |
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Geologi, hidrologi & meteorologi Daniel Adipradipto, GEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA |
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Java is a familiar area to many interest of geology including oil and gas
exploration. The Rembang-Madura-Kangean-Sakala (RMKS) area is one of the
most common studied area in East Java. This research area covers Blora and
Rembang district. Research area covering about 66 km2 is composed to six
formations, according to Peta Badan Geologi. Researcher found six litology units
which can be differed descriptively in the field, they are Limestone I, Sandstone,
Limestone II, Claystone, Limestone III, and Marl unit. These six units are Early
Miocene to Holocene Age. The study area also has some geological structures, they
are fold, strike-slip fault, normal fault, and faultbend fold. There is also a study of
provenance of sandstone of Ngrayong Formation. Eight samples are classified as
Recycled Orogen Provenance (Dickinson and Suczek, 1979). |
format |
Final Project |
author |
Daniel Adipradipto, |
author_facet |
Daniel Adipradipto, |
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Daniel Adipradipto, |
title |
GEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA |
title_short |
GEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA |
title_full |
GEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA |
title_fullStr |
GEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA |
title_full_unstemmed |
GEOLOGY AND PROVENANCE OF FM. NGRAYONG SANDSTONE OF NGIYONO AND SURROUNDINGS, BLORA DISTRICT, CENTRAL JAVA |
title_sort |
geology and provenance of fm. ngrayong sandstone of ngiyono and surroundings, blora district, central java |
url |
https://digilib.itb.ac.id/gdl/view/26363 |
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