bab iv sedimen non k..

PEMERIAN NON CALASTIC
SEDIMENTARY ROCK

PEMERIAN BTN NON KLASTIK BASED ON:
Texture, and composition MINERAL
STRUCTURE:
Texture
1.KRISTALIN consists of Kristal-Kristal THE
INTERLOCKING, namely KRISTALNYA
Sharing Lock SAMA ONE OTHER.
2.AMORF: Comprising MINERAL NOT
Establish Kristal-Kristal AMORF OR.
NON KLASTIK STRUCTURE
Reaction form PROCESS OF CHEMICAL OR ACTIVITY Organic
MACAMNYA BETWEEN OTHER:
1.
FOSSILIFEROUS: STRUCTURE shown by OR IS fossil fossil consists of a composition (sediment
organic)
2.
OOLITIK: STRUCTURE WHERE A fragment KLASTIK veiled BY MINERAL NONKLASTIK, are
KONCENTRIS with the diameter <2mm
3.
PISOLITIK: SAMA OOLITIK BUT THE SIZE OF LARGE DIAMETERNYA MORE 2mm.
4.
ONKRESI: SAMA KENAMPAKAN STRUCTURE WITH THIS STRUCTURE OOLITIK BUT IS NOT
showed concentric nature.
5.
Cone in Cone: STRUCTURE PADABATUGAMPING KRISTALIN refers to the growth cone
PERKERUCUT.
6.
BIOHERM: BY organisms composed Pure and INSITU.
7.
BIOSTROM: BUT AS BIOHERM are KLASTIK. BIOSTROME is BIOHERM AND STRUCTURE OF
FOREIGN FIELD IN only appear.
8.
SEPTARIA: similar KONKRESI BUT HAVE LEMPUNGAN composition. Something special
REKAHAN IS - THAT REKAHAN Disorders Depreciation RESULTING MATERIAL-MATERIAL
LEMPUNGAN IS BECAUSE THEN THE PROCESS Dehidrasi midst that filled Kristal-Kristal BY
carbonic of coarse.
9.
GEODE: cavity-RONGA Kristal BY charged that grow toward the hollow CENTER IS.
10.
STYOLIT: CONNECTING THE BEGERIGI ANTAR Butir.
NON KLASTIK SEDIMENTARY ROCK MINERAL
COMPOSITION
VERY Simple MINERALNYA composition that is
consisting of one or two types of MINERAL
SAJA:
EXEMPLARY:
 BATUGAMPING: KALSIT, dolomite
 CHERT: KALSEDON
 Gypsum: Gypsum MINERAL
 ANHIDRIT: MINERAL ANHIDRIT.
