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Marl
Marl
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Blueschist
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Marl
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Blueschist

Formasi Marl lan Blueschist
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1 Tatanan
1.1 tatanan
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.
Wangun blueschist amarga metamorphism saka basalt lan rocks liyane karo komposisi padha ing tekanan dhuwur lan kurang Suhu lan kira-kira cocog kanggo ambane saka 15 kanggo 30 kilometer lan 200 kanggo 500 ° c.
1.2 komposisi
1.2.1 isi Mineral
kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz
albite, chlorite, epidote, garnet, glaucophane, lawsonite, muscovite utawa illite, quartz
1.2.2 senyawa isi
aluminium oxide, NaCl, cao, wesi (iii) oxide, silikon dioksida
aluminium oxide, cao, wesi (iii) oxide, feo, kalium oxide, MgO, keda, sodium oxide, fosfor pentoxide, silikon dioksida, titanium dioxide
1.3 transformasi
1.3.1 metamorphism
✔ ✘
19% Sedimentary Rocks rocks have it !
✔ ✘
97% Igneous Rocks rocks have it !
1.3.2 jinis metamorphism
ora ditrapake
ora ditrapake
1.3.3 cuaca
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78% Sedimentary Rocks rocks have it !
✔ ✘
99% Igneous Rocks rocks have it !
1.3.4 jinis udan
udan biologi, udan kimia
udan mechanical
1.3.5 erosi
✔ ✘
86% Sedimentary Rocks rocks have it !
✔ ✘
92% Igneous Rocks rocks have it !
1.3.6 jinis erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi

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