Analysis of Pumice Thickness Layers As a Result of Rinjani Volcano Eruption in Lombok Island Based on Resistivity Data
Pumice deposits as a result of eruption of Rinjani volcano in Lombok Island, where it spreads and the thickness of the layers are not clear yet (hypothetically only). One of powerful method is used to determine the thickness of the pumice layer by using resistivity method. The purpose of this re...
محفوظ في:
| المؤلفون الرئيسيون: | , , , , |
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| التنسيق: | Conference or Workshop Item PeerReviewed |
| اللغة: | English |
| منشور في: |
2013
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| الموضوعات: | |
| الوصول للمادة أونلاين: | https://repository.ugm.ac.id/96944/1/6.pdf https://repository.ugm.ac.id/96944/ |
| الوسوم: |
إضافة وسم
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| الملخص: | Pumice deposits as a result of eruption of Rinjani
volcano in Lombok Island, where it spreads and the thickness of
the layers are not clear yet (hypothetically only). One of powerful
method is used to determine the thickness of the pumice layer by
using resistivity method. The purpose of this research is to
analyze the thickness of the pumice layer by the resistivity data.
The result indicate that the fumice was found in all around of
Lombok island (in East, North, Central, West, and South
Lombok, respectively). The thickness pumice layers have a
variation between 1.2 - 50 m, and its resistivity values ranging
between 15-441 Ωm which is situated in 2 to 5 layers of each
locations. The variation of resistivity values and the number of
layers depend on location distance, both horizontal and vertical direction from the center volcano eruption |
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