GENESIS VULKANIK DAKAH BERUMUR TERSIER DI DAERAH KARANGSAMBUNG, KEBUMEN, JAWA TENGAH
The presence of Tertiary volcanic in the Karangsambung area are shallow intrusion of diabas and basalt andesitic, massive lava basaltic, pillow lava basaltic, pyroclastic tuff and hialoclastit breccia in situ and sedimentary. Field observations show that the shallow intrusions were formed in s...
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| 語言: | Indonesia |
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| 在線閱讀: | https://digilib.itb.ac.id/gdl/view/73037 |
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