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Marl
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Formasi Marl lan Batubara
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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 coal saka klempakan saka lebu tetanduran ing lingkungan rawa kang wis kakubur sedimen kayata lendhut utawa wedhi lan banjur compacted kanggo mbentuk coal.
1.2 komposisi
1.2.1 isi Mineral
kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz
analcime, apatite, barite, kalsit, chalcopyrite, chlorite, chromite, clausthalite, mineral lempung, grup crandallite, dolomite, Feldspar, galena, gypsum, marcasite, muscovite utawa illite, pyrite, quartz, siderite, sphalerite, zirkon
1.2.2 senyawa isi
aluminium oxide, NaCl, cao, wesi (iii) oxide, silikon dioksida
karbon, hidrogen, nitrogen, oksigen, belerang
1.3 transformasi
1.3.1 metamorphism
✔ ✘
19% Sedimentary Rocks rocks have it !
✔ ✘
19% Sedimentary Rocks rocks have it !
1.3.2 jinis metamorphism
ora ditrapake
metamorphism kakubur, metamorphism cataclastic, metamorphism regional
1.3.3 cuaca
✔ ✘
78% Sedimentary Rocks rocks have it !
✔ ✘
78% Sedimentary Rocks rocks have it !
1.3.4 jinis udan
udan biologi, udan kimia
ora ditrapake
1.3.5 erosi
✔ ✘
86% Sedimentary Rocks rocks have it !
✔ ✘
86% Sedimentary Rocks rocks have it !
1.3.6 jinis erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi
ora ditrapake

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