Fluid-Rock Interaction During Hydrothermal Alteration at Parangtritis Geothermal Area, Yogyakarta, Indonesia
Parangtritis Volcano is part of the Tertiary magmatic belt in Java, which was tectonically formed by collisions between the Eurasian Continental Plate and Indo-Australian Oceanic Plate. The collisions have taken place since Late Cretaceous and still continue until today. In that period, the magmatic...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Geological Agency
2019-01-01
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| Series: | Indonesian Journal on Geoscience |
| Online Access: | https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/353/276 |