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Marl
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Peridotite
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Peridotite

Formasi Marl lan Peridotite
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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.
peridotites bisa kawangun ing rong cara: minangka rocks lapisan kawangun sak accretion lan diferensiasi saka bumi utawa minangka rocks cumulate kawangun dening udan saka olivine lan pyroxenes saka magmas basaltic.
1.2 komposisi
1.2.1 isi Mineral
kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz
amphibole, chromite, garnet, Magnesium, olivine, phlogopite, plagioclase, pyroxene
1.2.2 senyawa isi
aluminium oxide, NaCl, cao, wesi (iii) oxide, silikon dioksida
ca, fe, mg, kalium, silikon dioksida, sodium, titanium dioxide
1.3 transformasi
1.3.1 metamorphism
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19% Sedimentary Rocks rocks have it !
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97% Igneous Rocks rocks have it !
1.3.2 jinis metamorphism
ora ditrapake
metamorphism kakubur, metamorphism cataclastic, kontak metamorphism, hidrotermal metamorphism, impact metamorphism, metamorphism regional
1.3.3 cuaca
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78% Sedimentary Rocks rocks have it !
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99% Igneous Rocks rocks have it !
1.3.4 jinis udan
udan biologi, udan kimia
udan biologi, udan kimia, udan mechanical
1.3.5 erosi
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86% Sedimentary Rocks rocks have it !
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92% Igneous Rocks rocks have it !
1.3.6 jinis erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi
erosi kimia

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