Term
|
Definition
| The study of sedimentary and volcanic layers through time |
|
|
Term
|
Definition
| studying the rocks/what the rocks are made of in the layers |
|
|
Term
|
Definition
| studying the fossils within the layers of stratigraphy |
|
|
Term
|
Definition
| formation, group/comparitive, member, beds |
|
|
Term
| formation (main) division of stratigraphy |
|
Definition
| used to identify sequences of deposition |
|
|
Term
| group/comparative division of stratigraphy |
|
Definition
| used to compare depositional events |
|
|
Term
| member division of stratigraphy |
|
Definition
| used to identify individual depositional events |
|
|
Term
| bed division of stratigraphy |
|
Definition
| used to identify individual layers in a member |
|
|
Term
|
Definition
| comparing one rock to another to determine estimated age |
|
|
Term
|
Definition
| assigning a # to a rock when determining age |
|
|
Term
| principles of stratigraphy |
|
Definition
| original horizontality, superposition, lateral continuity, inclusions, and cross cutting relations. |
|
|
Term
| principles of original horizontinality |
|
Definition
| as sediments are deposited, they are laid out in horizontal sheets |
|
|
Term
| principles of superposition |
|
Definition
| when looking at a sequence, oldest rocks are at the bottom with the youngest at the top |
|
|
Term
| principles of lateral continuity |
|
Definition
as sediments are being deposited they will spread out laterally until 1. taper (thin out) 2. lean/touch a barrier 3. gradually change into another rock |
|
|
Term
|
Definition
any feature (Fragments, fossils) included in a rock must be older than the rock - also generated when magma intrudes upon a rock and breaks off |
|
|
Term
| principles of cross cutting |
|
Definition
| any feature (faults/igneous intrusions) that cut across stratigraphy must be younger than the stratigraphy it cuts |
|
|
Term
|
Definition
| missing geologic time, erosional surfaces, sometimes lock or deposition. |
|
|
Term
|
Definition
| disconformity, nonconformity, angular conformity |
|
|
Term
|
Definition
| missing time between parallel surfaces |
|
|
Term
|
Definition
| missing time between stratigraphy and an igneous or metamorphic body |
|
|
Term
|
Definition
| missing time between non-parallel layers |
|
|
Term
|
Definition
| age determination based on characteristics such as faunal succession and continuity |
|
|
Term
|
Definition
| utilizes the atomic decay of elements |
|
|
Term
|
Definition
| number of protons in a nucleus |
|
|
Term
|
Definition
| number of protons and neutrons |
|
|
Term
|
Definition
when ann element holds the same number of protons but varies in number of neutrons EX: Carbon = 6 protons Carbon Isotope (carbon 14) = 6 protons 8 neutrons. |
|
|
Term
|
Definition
| original radioactive element (will decay) |
|
|
Term
|
Definition
product of radioactive decay of parent isotope - can be stable unstable (unstable = radioactive) |
|
|
Term
|
Definition
| time required for half of the parent to decay to the daughter (can only date up to 5 half lives) |
|
|
Term
|
Definition
| the nucleus ejects 2 protons and 2 neutrons |
|
|
Term
|
Definition
| proton captures an electron, turning into a neutron |
|
|
Term
|
Definition
| neutron ejects an electron, turning into a proton |
|
|
Term
|
Definition
| change in form due to being exposed to conditions unlike those in which it formed |
|
|
Term
|
Definition
| heat, pressure, and fluids |
|
|
Term
| agents of metamorphism: heat |
|
Definition
temperature increases with depth (~20º-30º/km). The heating is slow, but the reaction to the heat is fast - can range as low as 200ºc up to 700º-1200ºC |
|
|
Term
| agents of metamorphism: pressure |
|
Definition
| 1000 atmosphers = 1000 bars = 1kbar = 3km in depth |
|
|
Term
| agents of metamorphism: fluids |
|
Definition
| H2O and CO2 act as catalysts and aid in the recystallization of minerals |
|
|
Term
|
Definition
|
|
Term
| low grade metamorphic rock |
|
Definition
| low temperature, low pressure |
|
|
Term
| intermediate grade metamorphic rocks |
|
Definition
| mid temperature, mid pressure |
|
|
Term
| high grade metamorphic rocks |
|
Definition
| high temperature, high pressure |
|
|
Term
| regional metamorphism characteristics |
|
Definition
-pressure driven (high temp/high pressure) -convergent boundaries (subduction and continental collision |
|
|
Term
| cataclastic metamorphism characteristics |
|
Definition
-occur on the fault -very rapid - high temp/high pressure |
|
|
Term
| contact metamorphism characteristics |
|
Definition
-contact with magma or lava -relatively small areas -high temp / low to moderate pressure -heat driven |
|
|
Term
| hydrothermal metamorphism characteristics |
|
Definition
-aka seafloor metamorphism -divergent boundaries -hot iron rich fluids |
|
|
Term
| burial metamorphism characteristics |
|
Definition
|
|
Term
| impact metamorphisms characteristics |
|
Definition
-instantaneous in heat/pressure -widest range in temp/area/pressure |
|
|
Term
|
Definition
| parallel alignment of minerals due to directed pressure |
|
|
Term
|
Definition
| slaty (shale, slate, phyllite) |
|
|
Term
|
Definition
|
|