Formasi Marl lan Claystone

Marl

Claystone

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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.

claystone iku umume cukup alus, nanging bisa dadi hard lan brittle. iku formulir amarga cuaca saka mudstone.

1.2 komposisi

1.2.1 isi Mineral

kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz

biotite, chlorite, Feldspar, micas, muscovite utawa illite, plagioclase, pyrite, quartz

1.2.2 senyawa isi

aluminium oxide, NaCl, cao, wesi (iii) oxide, silikon dioksida

aluminium oxide, ca, NaCl, cao, wesi (iii) oxide, MgO, silikon dioksida

1.3 transformasi

1.3.1 metamorphism

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19% Sedimentary Rocks rocks have it !

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19% Sedimentary Rocks rocks have it !

1.3.2 jinis metamorphism

ora ditrapake

1.3.3 cuaca

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78% Sedimentary Rocks rocks have it !

✔ ✘

78% Sedimentary 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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86% Sedimentary Rocks rocks have it !

1.3.6 jinis erosi

erosi kimia, erosi gisik, banyu erosi, angin erosi

erosi gisik, banyu erosi

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