Serpentinisasi Pada Batuan Ultramafik dan Implikasinya Terhadap Eksplorasi Endapan Nikel Laterit
<p>Serpentine is a group of magnesium hydro-silicate mineral (Mg3Si205(OH)4) that formed through hydration reaction of ultramafic rock with olivine and pyroxene as the main phases. Three serpentine minerals may be distinguished on the basis of their morphology as platy lizardite, fibrous chrys...
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| 格式: | Article NonPeerReviewed |
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[Yogyakarta] : Departemnts of Geological Engineering Faculty of E
2009
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| 在線閱讀: | https://repository.ugm.ac.id/95190/ http://repository.ugm.ac.id/digitasi/index.php?module=cari_hasil_full&idbuku=3008 |
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