Sedimentary Rocks Lab Flashcards
Two sedimentary textures
Crystalline texture (crystals grown together) and Clastic texture (“aggregate of grains”; rocks cemented together)
How does a clastic sedimentary rock form?
Clastic rocks come from loose, unconsolidated aggregate of mineral grains and rock fragments and subsequent cementation (gluing together) and compaction (squishing)
How does a chemical sedimentary rock form?
Chemical sedimentary rocks form from the precipitation of minerals out of solution (sea, water, lakes, etc). Common chemical sedimentary rocks are limestone and rock salt.
Framework
Packed clasts that are in partial or full contact with one another (basically the big rocks in sedimentary rocks that are held by the matrix and cement)
Matrix
Consists of smaller grains that fill spaces between the larger framework grains
Cement
Binds the framework and/or matrix grains to form sedimentary rocks. Cements form when a water-based solution is present within the pore space of sediment and minerals precipitate from this solution, partially or entirely filling the pores between sediment grains. The most common types of cement are quartz (silica), calcite, dolomite, hematite, and clay minerals
Pore space
Non-solid space between grains that is filled with fluid (air, water, oil, natural gas)
Conglomerate vs breccia
Conglomerate has rounded clasts and breccia has angular clasts. In both cases, clasts have to be 2 mm and larger, otherwise the rock will be considered a sandstone.
Granule
2-4 mm
Pebble
4-64 mm
Cobble
64-256 mm
Boulder
more than 256 mm
Two types of clay
Mudstone (if massive) or shale (if fissile)
Naming sedimentary rocks
When naming any sedimentary rock, it is very important to remember to include a grain-size modifier for the dominant clast size.
3 types of roundness
Very angular, subrounded/subangular, well rounded