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