Lecture 2 Flashcards
beds to sedimentary basins
lithostratigraphy
biozones and stratigraphic ranges
biostratigraphy
reversals and polarity chrons
magnetostratigraphy
LOWESS 87Sr/86Sr ratio curve
chemostratigraphy
orbital eccentricity cycles
cylcostratigraphy
igneous rocks such as granites formed from melts deep underground (–) or above ground in the form of lavas and tuff (volcanic rocks)
plutonic
metamorphic rocks such as slate, marble, and gneiss formed by – and another kind of rock
heating and/or squeezing
examples of sedimentary rock
shales and sandstones
sedimentary rock are formed of materials transported by water and/or wind and deposited in areas of –
low potential energy (sedimentary basins)
– is concerned with the order of deposition of sedimentary rocks
stratigraphy
lithostratigraphy involves the recognition of – which are features on geological maps
rock units
sedimentary rocks are deposited in layers called –
bed or laminae
– consist of a succession of similar beds or an alternation of two or a few different types
rock units
basic rock unit
formation
fromations may lie on continents (epicontinental) or at the edges of the continents or –
sea floor
sea floor spreading followed by – limits the age of ocean basin deposits to less than about 150 Ma
subduction
T/F: 300 Ma Australia was much farther south
true
Nowra Sandstone is resistant to erosion so it’s a – sandstone
cliff forming
longshore drift causes quartz to move – along the Burdekin River
northward
total duration of any taxon from first to last individual is called the –
biozone