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made of preexisting rocks classified based in composition, grain size, texture |
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made of organisms organisms made shells from dissolved componets |
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preciptated inorganically from water evaporates, limestone |
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biogenetic and chemical sedi rocks classified based on 2 |
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mineroligy orecipitatin mechanism |
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bio activity alters water so minerals DIRECTLY precipitate |
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organic rock production mechanism |
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deposits very full if organic matter such as coal |
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what does the age of a rock tell you 3 2 eg of specific helpful sediments |
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geoloic history and relationships aids in relativ age dating BIOSTRATIGRAPHY
interbedded ash and volcanic units detriatal zircons - radioisotpes |
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provenace of rocks 3 2 eg to use |
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Definition
the source of sediment geologic history sediment basins can record the erooded rock;s history
detrital zircons paleocurrent indicators |
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environment of deposition can tell you 3 3 eg to look for |
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paleogeography paleoclimate paleobiogeography
sediment textures minerology fossils |
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physical and chemical changes that change sediment into a sedi rock occurs after deposition |
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geochem of rocks can tell us 4 2 eg of tools to use |
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correlation of strats paleoclimate interpretations record poist deposition diagenisis record of bioactivity in the environment |
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allignment of sedimentatry rocks with the flow diorection of a current passing over it |
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5 steps for forming sedi rocks |
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begin with source rock weathering - loss of chemically unustale species transpo - increases rounding, loss of mech unstable species deposition - produeces stratification, sorts by size, density, often addds chemical species diagenisis - authigenisis, cementation, compaction |
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process whereby a mineral or sedimentary rock deposit is generated where it is found or observed. |
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physical - mech breakdown chemical - rxns change rock composition bio - with aid by/ perpretraited by organisms, bio acids, root wedging |
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physical weathering 4 examples |
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by wind water ice thermal stress - alternating hot/ cold frost wedging unloading |
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chem weathering 3 expamples |
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rain dissolution by H2CO3 (chem weathering in this way is earth';s thermostat - increased sedi of rocks = lower T) hydrolysis - can turn fspar to clay oxidation - controls oxygen concentration |
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o horizon - loose decaying org matter a - minerals and humus e - eluvation zone (transpo of dissolved species by rain water), leeching b - clays c - partially altered parent material unweahered parent material |
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soil layers - depend on ______ 2 other points |
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depends of precipitaion dry = clasys wet = thick and well devoloped with saprolite
bacterial and org breakdown of rocks for increased nutrients
paleosoils |
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ancient soil used ot reconstruct surrface |
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removal of weathered material |
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dimensionless large Re = turbulent small Re = laminar |
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mue (crazy u) - viscocity v - velocity of fluid r constant p = density |
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V=Cd^2 v = settling veloc c = drag coeffient d = particle diameter |
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2 ways sedi moves in river |
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suspension saltation - bouncing along floor |
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sedi gravity flows 3 2 types with exaples |
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Definition
very rapid transpo very large quantities of sedi very coasrse sedi
subarial - debis flows subaquesous - turbidity currents |
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6 types of sedi gravity flows |
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grain flow fluidization liqifaction debris/ mud flow debis avalanche turbidite |
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4 most imprtnat gravity flows |
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grian glow fluidization debris flow turbidite |
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mass of dry cohesionless sedi by gravity no water needed |
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grains supported by water upward motion of escaping fluid |
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sedi looses strength and cohesion due to appleied stress like and EQ behaves like a liquid |
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supported by cohesive mud matris poorly sorted mis of sedi and water steep slopes needed fast flow |
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grain suport mechanism is turbylence more fluid flow than grain flows decrese in slope stops the flow gravity driven |
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processes occuring now over extrmeely ,ong time period explain the geologic record |
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short term violent massive global scale events shaped geologic record |
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primary sedi structures 2 |
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physically created during transpo and deposition define environments |
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secndary sedi structures 5 |
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physical or bio created occur after initail deposition of sedi sometimes diagnostoc soft sedi deformation post depositional |
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unideriectional currents 2 |
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water flows one way making diagnostic features man generate x beds (sediment is pushed up hill and down into valley filling the valley) |
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occur in specific tidal areas herringbone x strat - equal power water flows |
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secondary sedi structures examples 3 |
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ball and pillows flame strucutres cokvulte bedding - complex folding of laminations |
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paleoenvironmental interpretations define inchnofacies |
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assembly of fossils that gives conditions an organism may have inhabited |
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sandst formed from resistant rock area of heavy decomposition (river channel, warm wet environ) often thin deposits |
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made up of many types of rokcs thick deposits erroded from high relief sources |
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qtz arentite fspar areneite lithic arentie wacke |
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most common sandst not evenly distributed in time formed from intense weatherinf of stable cratons |
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low sorting and less mature common at continental normal faults formed from less intense weathering than qtz areneite |
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common in orogonic wedges |
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common in turbidity flows dominant sandst of the archean |
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area of increasseing mountain height over subducting crust |
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clays 2 2 types 2 common names |
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phylo silicates with tetra and octa layers aqueous environs
type 1 - ot-ot layers typer 2 - tot-tot layers with interlayers cations tha tattract water (more charge = more water)
monmorillinite - swells illite - no swelling |
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abundant in reored anoxic coniditions high concntrations of organic matter |
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anoxic fossil beds that limiy decomp of organisms "storage place" exceptional fossil preservation |
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everything after dep and before metam chem phys, bio proccessing compaction 0 reorganize grains to more compact structure lithification |
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gaps with no matris
interconnectedness of pores |
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compaction - clast deformation and distorotion decrease permiability and porosity caused by increased p due to burial pressure dissolution |
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precipitate form in cracks, proes around grain edges
styolites |
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minerials precipitate from pore fluiods variable formation times effects - lithification - binds clasts large decrease in porpsity |
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common cements in sand stones 3 |
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calcite - very soluble and very common - near surface where small changes in pH hav large impact on doissolution
qtz - less soluble but increases with increasing T
Iron oxides - red - dissolves in reducing environs (low O) - quick precip in oxic environs |
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carbinate cememts 2 3 eg and locations |
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readily occurs in deposition and burial depth and water composition has large impact on type of cement
arag/ calcit
dolomite at depth |
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new minerals created from recycled elements and minerals
alteration of clays hematite forms from FeO minerals |
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diff mineral preipitates in previuosly occupied space needs dissolution of orginal precip of new
petrified wood - replaced by chert |
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existing minerals grow larger very common in carbonates (may obscure orginal texture) |
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deporitional environ sequence 4 |
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fan shaped coarse with poor sorting formed at sharp topgraphic boundries has b riv channels throughout it |
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a fan formation caused by located at how thick |
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majoir change of slope causes hydraulic pressure to decrese rift valleys, grabens, fareland basins km thick |
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streams, floods b riv gravity, debris, mud plants may occupy space increasing stability |
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coasre up distal x beds unsorted debris immature sedi |
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stream discharge cant carry all sedi in it |
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favour b riv over m riv when 3 |
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high errosion coarse sedi low or varied discharge |
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associated with fast up life/ down dropping basins fine upwards low mud, high sand and cobble cincentratins l and t bars |
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further from the source energy goes to cutting laterally not into bedrock bc of flat topography long ribbon sands entranched m riv from uplift |
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floodplain point bar channel |
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lake fine sedi fine laminations often with seasonal bio sedi fresh water may have wierd chem organic rich |
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river spreads at sea, bars form, river splits fining away from river mouth sheltered locals at river dominated - more side than errosion at wave dominated - sedi moves parallel to shore tends to prpograde - coasrse up |
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sequence strat untip - downdip - |
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Definition
link sedi packs that are bound by correlative conformities and unconformities
to source
to basin |
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relate time of dep
similar rock types
they are used in tandem |
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sequnnce boundry cause = 2 types |
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sea level fall
below slope = shelf break no shift in relative shoreline position |
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set of beds bound by marine flooding surface causeed by sea level rise (eusatic) coarsen up with abrupt shoft to fine grain facies depositedin lateral continuity |
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vertical succession of sedi units caused by lateral change in depositional environ
lateral change in lithology in correltave units reflect horizontal change in dep environ |
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Highland sys tract sedi accumulation faster than accomodation |
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transgressive system tract onset of coastal transgression |
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lowland system tract after sea level rise |
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separates TST from Hst Deepest water facies in unit |
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Marine dep environs near and far shore |
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n - coarse, turbidites (buoma sequences) f - finer dominated by bio sedi and marine snow |
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silicious ooze - bio orgs that make shells of silica calacreous sedi |
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connect 2 larger water bodies as elongate passages amplify currents bc of constriction only small sea surface elevations needed for storng surrents flow modified by channel obstructions |
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large scale x beds sandstx bedding without mud drapes (Mud drapes are found in deltas) trace fossils shoould refelct marine salinity levels |
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how does sea level influence velocity |
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hoigh sea level decrsae constriction decrease v increase sedi accomodationm space
may cause low e deposits over high e |
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use fossils for age dating |
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rock at bc latitudes originally formed in baja CA? paleomag data suggests low lat formation lack of large scale geo evidence for transpo however |
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1 rocks formed at current lat, no need for long transpo
2 paleomag data suggest soem rokcs have paleomag data for low lat. need to travell long distance in short time |
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zone just above high tide to just bellow low tide |
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3 main carb dep environ dimensions of deposits |
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bahamas arabian peninsula warmer = higher dep laterally extnsive, not thick |
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normal salinity well mixed (oxygenated) bioturbation common bioherm in high e environ |
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ancient reef made of organic structures |
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form at the edge of carbonate platform record the chem of the ocean |
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record ocean chem by
what 4 things cna you nmeasure |
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analzing the precipitates form the ocean like carbonates
O and C isotopes T Atmos CO2 |
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stable isotopes may cause____ which may depends on______ |
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diff in mass cases diifferent behavior frctionation temperature, easy of uptake into bio proceesses |
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relative abundance of an isotope compared to a standard |
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photosyth preferentially uptakes 12C over 13C leavign ocean high in 13C |
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boron isotopes 2 absundance of isotopes based on |
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B(OH)3 as boric acid B(OH)- as borate same size and charge as carbononate minerals. can easilt substitute contoilled by pH and fractionations |
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thin isochronus - laid down at same time conspicuos wide spread
volc ash, fossils of massive die off |
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1 major eustatic cycles caused by super cintentnt breakup/ formation
2 eustatic cycles induced by volume changes in MOR systems
3 crustural flexures
4 rapid eustatic fluctuations bc ice cheet growth/ decay and delta growth/ decay |
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pump enmergy into ground, diff ltih units have diffeernt seismic v so can map the refractions |
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conformabel succession of related strata bound by conformitoes and unconformities |
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conformable successions of beds bound by marine flooding surfaces |
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accomodation space is grater than sedi supply |
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sedi supply greater than accomodation space |
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sedi supply is about equal to accomodation space |
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accumulation of km of thick sedi long livede need lonng term subsidence to create accomodation space |
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topography is a function of litho density |
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topography a function of litho thickness |
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ridgid astheno can act as an elastic plate flaxes when loaded |
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extensional boundry basins |
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rift basins ultimately passive margins driven by crustal thinning and heat flow of astheno sphere beneath it |
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ocean contacting contintal litho that is not active |
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convergen boundry basins 3 eg |
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flexure of underlying plate by weight of overriding plate deepest at mountain fronts most accomodation space
forarc basins |
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pull apart basins heat lost thru walls so rapid fault controlled subsidence rapid lateral facies variations |
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1 continental rift at spreading centre 2 new oceanic crust at seaflor spreading centre 3 ocean basin with MOR and passive margins 4 passive margin becomes active, oc subd under cont 5 continued subd, MOR closes 6 cont crust from either side of MOR colides |
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sedi packages and mountain beslts the vesult of vertical motion now we know horizontal techtonics dominate |
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geocynclinal theory past view |
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sedi accumulation occured in lond troughs |
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geocynclinal theory presnt wiew 5 |
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sedi weighs down crust increasing subsidence and sedimentation folds and faulting mnts where thick sedi deposited uplift from contraction of cooling earth and sedimentation shifting to oceans |
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accomadation space created at tech spreading centers how? conv 2 div 2 transform 1 |
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Definition
c - crustal flexing and faulting d - faulting, thermal subsidence t - faulting |
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intracratonal basons cause of subsidence 3 |
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underlysing rifts cooling after intrusions of dense material downwelling from cold spots |
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edvidence for the appearance of Oxygen 4 |
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dissapearnace of detrital pyrites, BIFs, Sulfur MIF
appearance of redbeds |
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grain flow rock record evidence 3 |
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no grading massive deposits grain orientation parallel to flow |
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fluidized flow rock record evidence 4 |
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convolute laminations on top fluid escape structures like pipes, flames poor grading flame and loading structures |
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debris flow rock record evidence 4 |
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irregular top with grains projecting poor sorting poor grading scours at base |
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turbidity current rock record evidence 3 |
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micro cross laminations good grading laminated |
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failed rift valley (3rd leg) |
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what age with a detrial zircon give you? |
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thin sedi packages found in what basin |
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an abundant and characteristic fossil |
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sequences that represents a rapid deepening of water deoth |
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zachos oxy isotope curve records |
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change in abundance of carbon isotopes in carbonates represents |
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most common mineral in sandstone |
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why are black shales black? |
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ratio of inertial force to gravatational force |
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characteristics of primary sedi structure 3 and ine that is not |
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occur in clastic rocks porodiced by currents reflect transpo and depo features
not bio activity |
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do trace fossil assemblages give the organism that made the fossil? |
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thickness of a lamination |
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most preserved volume of sedi found in what eon |
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fast chem weathering by 2 |
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