DOC PREVIEW
WVU GEOL 285 - Limestones and Dolomites

This preview shows page 1 out of 4 pages.

Save
View full document
View full document
Premium Document
Do you want full access? Go Premium and unlock all 4 pages.
Access to all documents
Download any document
Ad free experience
Premium Document
Do you want full access? Go Premium and unlock all 4 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

Geol 285 - Dr. Helen Lang, West Virginia University, Spring 2009Limestones and DolomitesCarbonate rocks, usually deposited with the help of biological organismsMineralogy is simple-Carbonate minerals: -Calcite CaCO3 -Aragonite CaCO3 -Dolomite CaMg(CO3)2 -Minor Quartz and/or ClayTherefore, Particle Types and Textures are Important for Classification- Allochemical Particles (allochems) - framework grains of a mechanically deposited limestone - four main types - some formed of calcite, some aragonite - Orthochemical Particles (orthochems) - matrix and cement that fill spaces, bind allochems together and lithify sedimentAllochems- Fossils - solid carbonate remains of organisms (fossils), and fragments of fossils- Peloids - ellipsoidal aggregates of micro-crystalline CaCO3, lack internal structure, mostly fecal pellets of worms, fish, etc. - Oöliths - spherical polycrystalline carbonate particles of sand size, with concentric or radial internal structure, commonly have a nucleus for precipitation - Limeclasts - fragments of earlier-formed limestone, mostly intraclasts from a localsourceFossils - Brachiopod ShellFossilsPeloidsOöidsOrthochems- Microcrystalline Calcite (Micrite) - CaCO3 mud, disarticulated algal material, carbonate ooze, 1- 4 -m diameter [Note difference between lime mud and silicate mud] - Coarsely crystalline calcite (Sparry calcite or "Sparite") - calcite cement, precipitated from pore fluid (inorganic ppt.) - Usually one or the other, not bothMicriteSparite=coarse crystalline calcite (Cc is stained pink)Non-carbonate Minerals- Typically less than 5% terrigenous detritus (quartz, clay, chert) - Limestones form only where input of terrigenous detritus (especially mud) is minimal: fresh water changes salinity, organisms are killed or buried by mud - Chert is intrabasinal from siliceous organisms or is diageneticGulf of MexicoLimestones occur where clastic input is minimalThere are two commonly used classification schemes• Folk’s Classification– Based on major allochem and major orthochem– Hard to use without thin sections– Not useful in the field• Dunham’s Classification– Based on structure and percent grains vs. mud– More useful in the fieldFolk’s Classification- Major Allochem (prefix) Major Orthochem (suffix) - Fossils bio- -micrite - Peloidspel- -sparite - Ooliths oo- - Limeclasts intra- - >90% micrite is just called MicriteFolk Name? BiomicriteFolk Name? OospariteFolk Name? MicriteDunham: field classification (see


View Full Document

WVU GEOL 285 - Limestones and Dolomites

Download Limestones and Dolomites
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view Limestones and Dolomites and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view Limestones and Dolomites 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?