paper 2 Flashcards
Diagenesis definition
the chemical and physical processes that turn sediments into sedimentary rocks
Diagenesis processes
1) cementation - infill of pore spaces by mineral cement
2) compaction - sediments squeezed by overlying sediment which decreases porosity and permeability
3) recrystallisation - crystals change in size and shape
4) dissolution - minerals dissolve where grains press into each other.
siliclastic rocks
silica based rocks such as mudstone and sandstone
methods to improve a dame site
Grouting - drilling hole and pumping in liquid cement to reduce porosity and improve stability of faults.
construct barrier underneath dam - prevent leakage underneath keeping it more stable
how does temperature affect silica content of magma and why
silica content increases as temperature decreases due to fractional crystallisation which crystalises some contents of the magma which causes the silica to be more strong in the remaining mixture.
How does silica affect magma
increased viscosity, - therefore divergent plate boundaries are mafic which produce shield volcanoes and convergent plate boundaries are silicic which create strata volcanoes.
what is the focus
point inside the earth where the earthquake occurs
what are ripple marks
sedimentary structures which indicate agitation by water
what are carbon films
thin coatings of carbon
mechanism of preservation resulting in carbon films
1) soft organism contains organic carbon
2) burial
3) subject to load pressure
4) causes increased temp and pressure
5) increased carbon % leaving carbon coating
epifaunal/infaunal definitions
epifaunal - lived attached to the surface
infaunal - live in the sediment eg in burrows
process of trilobites growing
1) cephalon breaks along facial structure
2) soft body exits the exoskelaton
3) it is vulnerable until new exoskelaton hardens
sedimentary basin
low lying area in the earths crust where sediments accumulate
how can the geometry of a sedimentary basin be determined
1) seismic surveys
2) correlation of sediments
isochemical
having a constant chemical composition