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The lateritic nickel deposit is result of decayed of ultramafic rocks as host of Nisilicate. Generally it is at tropical until subtropical area. The influence of tropical in Indonesia made process of decaying intensively, with the result of that some areas in Indonesia have thick laterite profile (d...
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Main Author: | SYAH ANAK AMPUN (NIM 12103047), SYAIFUL |
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/12701 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
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