STUDI PALEOSEISMOLOGI AKIBAT BENCANA GEMPA BUMI DI ZONA SESAR KALIGARANG (KGFZ) DI SEMARANG
Earthquake in the past can study with paleoseismology. Kaligarang fault zone will record the event of<br />earthquake and result the sediment. The metode of research is detail field mapping and field excavation.<br />Evidence of paleoseismology in the filed, we find the sand boil and car...
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| Format: | Article |
| Language: | English |
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Diponegoro University
2012-08-01
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| Series: | Teknik |
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| Online Access: | http://ejournal.undip.ac.id/index.php/teknik/article/view/4815 |
| Summary: | Earthquake in the past can study with paleoseismology. Kaligarang fault zone will record the event of<br />earthquake and result the sediment. The metode of research is detail field mapping and field excavation.<br />Evidence of paleoseismology in the filed, we find the sand boil and carbon materials. We find two location of<br />sand boil near with reverse faults. Sand boil to precipitate at unit B Kalibeng Formation. Phase tectonic to<br />cause earthquake occure at late Miocene – Early Pliocene. |
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| ISSN: | 0852-1697 2460-9919 |