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Marl
Marl
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Formasi Marl lan Obsidian
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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.
nalika lahar dirilis saka gunung, iku diwiwiti saka cooling cepet banget kang freezes mekanisme saka crystallization. asil punika kaca vulkanik karo susunan Gamelan seragam.
1.2 komposisi
1.2.1 isi Mineral
kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz
ora kasedhiya
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
metamorphism kakubur, metamorphism cataclastic, kontak metamorphism
1.3.3 cuaca
✔ ✘
78% Sedimentary Rocks rocks have it !
✔ ✘
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
✔ ✘
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, erosi Glacier

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