Week 5 Flashcards
Carbonate minerals
Calcite
Aragonite
Dolomite
Calcite
CaCO3
Trigonal rhombohedral
Layered with central Ca2+
Most common in rock record
Aragonite
CaCO3
Orthorhombic
Metastable over 10-100s of million years - alters to calcite
Most common in corals/molluscs
More MECHANICALLY stable
Dolomite
Ca.Mg(CO3)2
Alteration of calcite - Mg from meteoric waters
More resistance to weathering (unless powdered b/c increases SA)
Buff colour due to Fe
Can have high Mg calcite but dolomite is 50:50
Types of allochems
Ooids
Peloids
Skeletal grains
Forms
Coccoliths
Ooids
= less than mm carbonate spheres, grow around a nucleus
Higher energy = concentric circles
Sheltered = radial
Peloids
= no internal structure, amalgamations of carbonate mud
Can be subdivided into pellets/intraclasts
More elongated than voids because haven’t rolled/nucleated in the same way
Forams
= structure that single-celled organisms leave behind
Round, smooth
More structured than ooids/peloids
Coccolith
= microscopic plates that form a coccolithophore
Major component of chalk
Types of autochems
Sparry cement/sparite
Micritic cement/micrite
Sparite
Forms from calcite in pore fluid; so saturated that can form without deforming grains
Acicular/fibrous/drusy/granular
Acicular =
needle-like
Fibrous =
Thicker than acicular but fibrous
Drusy =
void-filling and pore-lining cement
Quick precipitation due to high saturation of calcite
Later availability lower = slows down
= crystals of different sizes
Granular =
calcite cement with relatively equidimensional pore-filling small crystals