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Borolanite
Borolanite
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Marl
Marl
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Borolanite
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Marl

Formasi Borolanite lan Marl
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1 Tatanan
1.1 tatanan
borolanites sing kawangun amarga aktivitas igneous alkalin lan umumé kawangun ing wilayah dharatan crustal nglukis utawa ing zona subduksi cordilleran.
Wangun marl nalika partikel lempung banget nggoleki-grained sing setor ing banyu kang settles ing ngisor banyu badan lan compacted dening overlying endhepan; banyu meres metu lan Empu mbentuk rock marl.
1.2 komposisi
1.2.1 isi Mineral
albite, amphibole, biotite, cancrinite, Feldspar, hornblende, plagioclase, pyroxene, sodalite
kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz
1.2.2 senyawa isi
aluminium oxide, cao, wesi (iii) oxide, feo, kalium oxide, MgO, keda, sodium oxide, fosfor pentoxide, silikon dioksida, titanium dioxide
aluminium oxide, NaCl, cao, wesi (iii) oxide, silikon dioksida
1.3 transformasi
1.3.1 metamorphism
✔ ✘
97% Igneous Rocks rocks have it !
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19% Sedimentary Rocks rocks have it !
1.3.2 jinis metamorphism
metamorphism regional
ora ditrapake
1.3.3 cuaca
✔ ✘
99% Igneous Rocks rocks have it !
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78% Sedimentary Rocks rocks have it !
1.3.4 jinis udan
udan kimia, udan mechanical
udan biologi, udan kimia
1.3.5 erosi
✔ ✘
92% Igneous Rocks rocks have it !
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86% Sedimentary Rocks rocks have it !
1.3.6 jinis erosi
angin erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi

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