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Formasi Phonolite lan Batubara
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1 Tatanan
1.1 tatanan
phonolite sing kawangun amarga aktivitas igneous alkalin lan umumé kawangun ing wilayah crustal Continental nglukis utawa ing zona subduksi cordilleran.
Wangun coal saka klempakan saka lebu tetanduran ing lingkungan rawa kang wis kakubur sedimen kayata lendhut utawa wedhi lan banjur compacted kanggo mbentuk coal.
1.2 komposisi
1.2.1 isi Mineral
albite, amphibole, biotite, cancrinite, Feldspar, hornblende, plagioclase, pyroxene, sodalite
analcime, apatite, barite, kalsit, chalcopyrite, chlorite, chromite, clausthalite, mineral lempung, grup crandallite, dolomite, Feldspar, galena, gypsum, marcasite, muscovite utawa illite, pyrite, quartz, siderite, sphalerite, zirkon
1.2.2 senyawa isi
aluminium oxide, cao, wesi (iii) oxide, feo, kalium oxide, MgO, keda, sodium oxide, fosfor pentoxide, silikon dioksida, titanium dioxide
karbon, hidrogen, nitrogen, oksigen, belerang
1.3 transformasi
1.3.1 metamorphism
✔ ✘
97% Igneous Rocks rocks have it !
✔ ✘
19% Sedimentary Rocks rocks have it !
1.3.2 jinis metamorphism
kontak metamorphism
metamorphism kakubur, metamorphism cataclastic, metamorphism regional
1.3.3 cuaca
✔ ✘
99% Igneous Rocks rocks have it !
✔ ✘
78% Sedimentary Rocks rocks have it !
1.3.4 jinis udan
udan kimia, udan mechanical
ora ditrapake
1.3.5 erosi
✔ ✘
92% Igneous Rocks rocks have it !
✔ ✘
86% Sedimentary Rocks rocks have it !
1.3.6 jinis erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi
ora ditrapake

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