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UNC - PSYCH - 100
Evolutionary Psych 602: Exam 2Chapter 5 G&M- Consciousness- What is the function of consciousness?- What are the different meanings of consciousnessChapter 6 G&M: Emotion and Virtue chapter 15 Pinker, Keltner, Chapter 7Chapter 7 G&M: CognitionChapte
UNC - PSYCH - 100
HumanMating/SpecialTopics23:22Exam:DEFAQUESTIONbackgroundrateclassicalandopperatioonalconditioningandthe NEWwaysoflookingatitfromaquestioningperspectivehelpsusunderstandfroman evolutionarypointofviewBACKGROUNDRATEandTASTEAVERSIONtheyarenotequalallth
UNC - PSYCH - 100
2/22/2012:Eckmans16:12DevelopmentaldevelopmentResearchIdeasFakeemotionsvs.realemotionsRealsmilevs.FakesmilesLyingvs.notLyingEmotionalexpressionmayhavederivedfromdisgustWhywouldwefeeltheneedtocommunicatethesetootherpeople?Readingemotions maybeadap
UNC - PSYCH - 100
Chapter10Health23:21Chapter10:EvolutionaryPsychHealthMismatchHypothesis:Manyofourhealthproblemscomefromdifferencesbetweenour presentlifestyleandthatintheEEA.Problemsofhealthmaybecausedbytheresultof amismatchbetweenourevolvedcharacteristicsandourprese
UNC - PSYCH - 512
EvolutionaryPsychology16:05Chapter4:SensationandPerceptionExam:4questions,2samplestudyquestionsthatareonblackboard.About1015minoneachessayVerycomplexandhaveapointratherthanlookingThebestessaysaretheonesthatteachsomething.NeedtoshowOWNthoughts,conce
UNC - PSYCH - 512
Becky LynchPaper OutlinePsyc 512Topic:How do the peer relations of intellectually gifted children differ from those ofintellectually average children? Are the developmental processed different? Whatcategory of peer relations are gifted children most
UNC - PSYCH - 512
Research:OutlineDueTuesdayOctober18th(CanbeANYsubjectaslongasthemainfocusispeerrelationsandadolescence)Include23referencesfromhighqualityjournalsStatethemainthesisofthepaper(ex:whatisthepointofthepaper,howwillthis papercontributetotheexistingliteratu
George Mason - ECON - 206
Chapter 2Factors: How TimeFactors:and Interest AffectMoneyMoneyLecture slides to accompanyEngineering Economy7th editionLeland BlankAnthony Tarquin2-1 2012 by McGraw-Hill, New York, N.Y All Rights ReservedLEARNING OUTCOMES1. F/PandP/FFactors
University of Texas - E M - 319
University of Texas - E M - 319
University of Texas - E M - 319
University of Texas - E M - 319
THE UNIVERSITY OF TEXAS AT AUSTINDepartment of Aerospace Engineering and Engineering MechanicsEM 319 MECHANICS OF SOLIDSSPRING 2012SYLLABUSUnique Numbers:13875, 13880, 13885, 13890, 13891Instructor:Mark E. MearWRW 112, 471-4212, mear@mail.utexas.
University of Texas - GEO - 316P
WEATHERING AND SEDIMENTARY ROCKS1.Weathering The first step in the chain of processes that producesedimentary rocks. Process which acts at the earth's surface to decomposeand breakdown rocks.2.Erosion - The movement of weathered material from the site
University of Texas - GEO - 316P
Grain ParametersLecture OutlineI.Grain-size analysis & statistical parametersII.Sediment / Rock textural classificationIII.Grain shapeIV.Grain roundnessV.Textural maturityVI.Sediment / rock fabricReading Assignment: Boggs, Chapter 3Why Do Grain-S
University of Texas - GEO - 316P
Grain MineralogyLecture OutlineI.Crust compositionII.QuartzIII.FeldsparIV.Rock fragmentsV.Other grainsVI.ClassificationReading Assignment: Boggs, Chapter 5, p. 119-139Crust Composition: Rock TypeContinental Crust:Granite ~ 60% Feldspar,25% Qua
University of Texas - GEO - 316P
1So What do we need to knowFlow typesFlow processesHow these control sediment movement or control/influencesedimentationHow these are represented in the rock recordTo begin: What forces control the behavior of fluids:Inertial forcesGravitational
University of Texas - GEO - 316P
Cross-Bedding, Bedforms, and Paleocurrentsby David M. Rubin and Carissa L. Carter1Transport of sediment typically results in the spontaneousdevelopment of trains of repetitive bed topography.Low Froude-Number BedformsSimons et al., 1961, USGS Water-
University of Texas - GEO - 316P
Other Sedimentary StructuresLecture OutlineI.Macro-scale featuresII.Bed-scale featuresIII.Deformation structuresIV.Surface structuresV.Sole structuresVI.Biogenic structuresReading Assignment: Boggs, Chapter 4: 74-81, 91-116.1Macro-Scale Features
University of Texas - GEO - 316P
Rivers and River DepositsOther words commonly used to describe rivers and theirdeposits:(1) fluvial (Latin word for "river")(2) alluvial deposits for river deposits (from Latin "to washagainst)Class reading from Boggs, Principles ofSedimentology an
University of Texas - GEO - 316P
DELTASHerodotus (c. 400 BC): thought the alluvial plain at mouth of Nile looked like aBarrell (1912): described the ancient (Devonian) Catskill Delta and defined adelta as "a deposit partly subaerial built bya river into or against a body of permanent
University of Texas - GEO - 316P
ExperimentalMorphodynamicsExperimentalMorphodynamicsXES2002:BaselevelcyclesXES2006:Multiplesedimentsources1mXES2005:Lateraltectonicvariation1ExperimentalStratigraphyExperimentalStratigraphyXES06strikesection,x=3.4mdipsection,y=2.7mXES052Foss
University of Texas - GEO - 316P
Chemical Sedimentary RocksChert Amorphous Silica-SiO2 Precipitated abiotically or as biotic hardparts Marine and Freshwater occurrencesSalt Table salt: NaCl (Halite) Part of the Evaporative Sequence Relatively uncommon in ancient rocksBedded Hal
University of Texas - GEO - 316P
Carbonate MineralsElemental chemistry of carbonate rocks:1.Calcium (Ca2+)2.Magnesium (Mg2+)3.Carbonate Ions (CO3-)Principle components (minerals) of limestones and dolostonesTrace elements: concentrated into many organisms skeletal structures Mg, F
University of Texas - GEO - 316P
Modes of CarbonatePrecipitation inorganic thermodynamics and reaction kinetics Abiotice.g., marine evaporites Precipitates where bioticeffects are negligible Biotically Inducede.g., microbialite Precipitates where theorganism sets the processin
University of Texas - GEO - 316P
Components of a CarbonaterockSkeletal grainsMatrix< 0.03 mmPoresCementNon-skeletal grains1Carbonate Constituents:SkeletalTrends in Skeletal Carbonate Producers with Time distribution, abundance, & MineralogyReview of Major Carbonate Producers
University of Texas - GEO - 316P
Temporal Distribution of MajorFaunal GroupsCarbonate Producers:BrachiopodsLargely benthic, sessile organism; a fewspecies are infaunalLow-Mg calcite (LMC)superficially look like clams, but that are quitedifferent in their anatomyCommon in Paleozo
University of Texas - GEO - 316P
Non-Skeletal Grains Peloids Coated Grains ooids, pisoids, oncoids, rhodoliths Grain Aggregrates (grapestone) Mechanical Clasts intraclasts lithoclastsPeloids Peloids are small (< 2 mm) spheroidal or ovoid particlesof fine-grained carbonate mud t
University of Texas - GEO - 316P
Matrix = Lime Mud What is it? silt & clay-sized carbonate sediment (<62 m) Why is it important geologically? constitutes 50% of carbonate strata by volume How is it Formed? precipitation from seawater post-mortem decay of calcareous algae Biomecha
University of Texas - GEO - 316P
LAKE SYSTEMSUSC WEBUSC WEBUSC WEBUSC WEBUSC WEBUSC WEBDESERT LAKES FORMED BY WIND DEFLATIONCRATER LAKE, OREGON, USALAKE FORMED BY VOLCANIC CRATER COLLASPE,CRATER LAKE, OREGONUSC WEBLACUSTRINE SYSTEMSCLOSED LAKE SYSTEMSTEMPERATURE OR CHEMICAL
University of Texas - GEO - 316P
DEPOSITIONAL SYSTEMSSHOREZONE SYSTEMSBARRIER BARS/LAGOONSSTRANDPLAINSCHENIERSTIDAL FLATS AND MUD FLATSGalveston/Bolivar Barrier Islands Texas CoastUSC WEBFORMING THE SHORE ZONEPROFILESAME FOR BARRIER BARAND STRANDPLAINUSC WEBUSC WEBUSC WEBU
University of Texas - GEO - 316P
REVIEW SESSIONTHINGS TO REMEMBERFISHER PRESENTATIONS FORSECOND QUARTER EXAM; ALSOPOSTED ON BLACKBOARDKIM PRESENTATIONS LAST WEEK;WILL BE INCLUDED ON EXAM; REVIEWPOSTED ON BLACKBOARDLACUSTRINE SYSTEMSTHINGS TO REMEMBERHOW LAKES FORM- DIFFERENT TY
University of Texas - GEO - 316P
REVIEW SESSIONTHINGS TO REMEMBERFISHER PRESENTATIONS FORSECOND QUARTER EXAM; ALSOPOSTED ON BLACKBOARDKIM PRESENTATIONS LAST WEEK;WILL BE INCLUDED ON EXAM; REVIEWPOSTED ON BLACKBOARDLACUSTRINE SYSTEMSTHINGS TO REMEMBERHOW LAKES FORM- DIFFERENT TY
University of Texas - GEO - 316P
123CONTINENTAL SHELF, NORTH AMERICANOTE BROAD SHELF ON EAST AND NARROW SHELF ON WEST4SEDIMENT WEDGE BELOW SHELF FORMED BYPREVIOUS PROGRADING COASTAL SEDIMENTS56SHELF SYSTEMS WAVE DOMINATED SHELVES TIDE DOMINATED SHELVES CARBONATE SHELVES AND
University of Texas - GEO - 316P
STRATIGRAPHY: HOWSEDIMENTS ARE ORGANIZEDFUNDAMENTAL CONCEPTS1WILLIAM (STRATA) SMITH(Somersetshire Coal Company1769-1839)FATHER OF STRATIGRAPHYStratigraphy = Study of rock strataThese strata preserve an integrated response of depositional systems
University of Texas - GEO - 316P
SEISMIC STRATIGRAPHYGEO 316PUSING REFLECTION SEISMIC TO RECOGNIZEDEPOSITIONAL SEQUENCES AND PACKAGESBY THE USEGEOMETRIC CONFIGURATIONS ANDTERMINATIONS OF SEISMIC REFLECTORSAND RECOGNITION OF SEISMIC SURFACES1SEISMIC ACQUISTION2TRAVEL TIME SEIS
University of Texas - GEO - 316P
SURFACE BOUNDARIES FOR SEQUENCESANDSTRATAL GEOMETRIES AND STACKINGPRODUCT OF BASE LEVEL CHANGE WHICHCAN COME FROM EUSTACY, SUBSIDENCE ORSEDIMENT INFLUX OR A COMBINATION OFALL THREESequence Stratigraphy That branch of stratigraphy which subdivides
University of Texas - GEO - 316P
MODERN CARBONATESSEDIMENTARY ROCKSGEO 316PModern Carbonate EnvironmentsBahamas, Isolated PlatformFlorida, Rimmed PlatformTrucial CoastArid RampModern Analogs for UnderstandingAncient ReservoirsModern CarbonatesBahamas Most studied modern carbo
University of Texas - GEO - 316P
SEDIMENTARYROCKSCARBONATESGEO316PEolian, Tidal Flat, and Shoreline SystemsTidal Flat and Shoreline SystemsModified from Loucks et al, 2004Major Facies Tracts in Shorezone SystemEolianTidalflatBarrierIsland/beach/tidalchannel/inletUpperandlowersh
University of Texas - GEO - 316P
316P Sedimentary RocksReef SystemsReefs Whataretheyandhowimportantarethey Classifications ReefDynamicsprocessesofreefdevelopment ReefSubfacies Stratigraphicsettingofreefs Coldwatervswarmwaterreefs ExamplesofreefoccurrenceandreservoirsReef Syste
University of Texas - GEO - 316P
GEO 316PCarbonate SlopesAttributes of Carbonate Slopes Dumping ground for shallow watersediments Different timing and sediment sourcethan for siliciclastic deposits Sediments deposited by combination ofsediment gravity flow processes Forms founda
University of Texas - GEO - 316P
Dolomite and DolomitizationGEO 316PSedimentary Rocks - CarbonatesOutline The Dolomite Problem Modern Dolomite Settings Dolomitization Reaction and GeochemicalRequirements Dolomite Textures Models for DolomitizationThe Dolomite ProblemRelative p
University of Texas - GEO - 316P
FUNDAMENTALS OFOIL AND GAS RESERVOIRSGEO 316PPROCESS OF BECOMING UTPETROLEUM ENGINEERS ANDYOUR MAIN JOB WILL BE TOGET THE MAXIMUM AMOUNT OFOIL AND GAS OUT OF ADISCOVERED RESERVOIRWE WILL DEVOTE 5 LECTUREPERIODSTO SHOW YOU HOW THISCOURSE IS MEA
University of Texas - GEO - 316P
DEPOSITIONAL SYSTEMS ANDRESERVOIRSGEO 316PConcept of depositional systems introduced byW. L. Fisher and J.H. McGowen (1967):3D assemblage of lithofacies genetically linked byactive (modern) process or inferred (ancient)process and events integratio
University of Texas - GEO - 316P
Sedimentary Rocks (GEO 316P)Spring 2012Lecture : Meets MWF 10-11 AM, JGB 2.324Instructors:Dr. William Fisher, wfisher@jsg.utexas.eduOffice: JGB 6.130, Office hours: MWF 1 3 PMDr. Wonsuck Kim, delta@jsg.utexas.eduOffice: EPS 3.154, Office hours: W 4
University of Texas - GEO - 316P
Ch. 16 Why is Carbonate sedimentology important? How do reefs and platforms get drowned in terms of Aggradation rate vs.Relative sea-level rise rate? Keeping up, catching up, and giving upCh. 17. Examples of carbonate sedimentary rocks Difference i
University of Texas - GEO - 316P
Sedimentology (2012)doi: 10.1111/j.1365-3091.2012.01321.xSea-level rise, depth-dependent carbonate sedimentation and theparadox of drowned platformsWONSUCK KIM* , , BRUCE W. FOUKE , ANDREW L. PETTER*, TERRENCE M. QUINN* , ,CHARLES KERANS* and FRED TA
University of Texas - PGE - 322K
PGE 322KTRANSPORT PHENOMENA INGEOSYSTEMS ENGINEERINGDr. Quoc. P. NguyenThe University of Texas at AustinCockrell School of EngineeringDepartment of Petroleum Engineering and GeosystemsShellIntroductionUnit systemUnit system used in this course:
University of Texas - PGE - 322K
An Introduction to RheologyBasic concepts and definitionsRheology: defined as the science of deformation and flowRheometry: concerned with measurements of stress and strain of materials insimple or complex deformation/flow geometry Simple deformation
University of Texas - PGE - 322K
Shell Momentum Balance for Steady Laminar FlowDefinitions of momentum fluxesMolecular momentum transfer Fluid at rest: static pressure p is due to momentum transfer amongmolecules in random motion. Fluid in motion: viscous stress is due to molecular
University of Texas - PGE - 322K
Equations of Change for Isothermal SystemsThe equation of continuity (or mass balance equation)Mass influx(inward arrows)Mass balance over a fixed control volume xy z y z u x x u x x x tyzx t xz u y u y yy y y x y u z z u z z z t ux u y u
University of Texas - PGE - 322K
Mechanisms of Energy TransferMechanisms of energy transferEnergy transfer by work p xx yx zx xyp yy zy xz yz p zz Energy influxes (inward arrows)yP(x,y,z)zxHeat sourcesEnergy outfluxes (outward arrows)Mechanisms of Energy TransferMech
University of Texas - PGE - 322K
Shell Energy BalanceEnergy conservation for homogeneous mediaEnergy influxes (inward arrows)yP(x,y,z)zxHeat sourceEnergy outfluxes (outward arrows) Energy balance for an unsteady-state systemRate ofenergy inRate ofenergy outRate of workby f
University of Texas - PGE - 322K
Non-isothermal Equations of changeEnergy conservation for homogeneous mediaTotal energy balance( E K U ) .( E K U )u .q t . p u . .u u.g SKinetic energy balanceEK . uEK . pu p .u . .u : u u.g tInternal energy balance( U ) .( U u ) .q p .u : u S
University of Texas - PGE - 322K
Homework Set #1:Due date: 26/01/12 by 11:00 PMProblem #1:Consider a spherical particle falling freely in a large fluid body. It is found experimentally thatthe terminal settling velocity u of the particle is dependent on: (1) particle diameter D; (2)
University of Texas - PGE - 322K
Homework Set #2:Due date: 02/09/12 by 11:00 amProblem #1:A thin plate of 30x60x0.1 cm3 size is falling vertically in a narrow slit as shown in Fig 1. Theplate thickness is assumed to be negligible as compared to the slit width of 1.5 cm. The slit isf
University of Texas - PGE - 322K
Homework Set #3:Due date: 02/16/12, by 11:00 AMProblem #1:Problem 2B.3 at the end of chapter 2 of BSL, parts (a), (b) and (c) only. Follow the terminologyin the diagram in Figure 2B.3 on p. 63. Note that x = 0 in the center of the slit in this figure.
University of Texas - PGE - 322K
Homework Set #4:Due date: 03/08/12, by 11:00 amProblem # 1:A Newtonian fluid fills a long cylindrical tube of radius R held vertically as shown. The tubewall is moving upward with velocity V < 0 (V is less than zero if the tube is moving up and z isd
University of Texas - PGE - 322K
Homework Set #5:Due date: 03/22/12, by 11:00 am.Problem #1:Solve problem 10.B.1 in BSL. Only questions a, b, and c.Problem #2:Read the statement of Problem 10.B.4 in BSL, but do NOT answer questions (a) and (b) in thetext. Answer the followings:(a)
University of Texas - PGE - 322K
Homework Set #6:Due date: 04/03/12, by 11:00 am.Problem #1:Solve Problem 3A.1 in Chapter 3 of BSL.Problem #2:The annular space between two coaxial long circular pipes is filled with a viscous, Newtonianfluid. The radii of the inner and outer wetted
University of Texas - PGE - 322K
Homework Set #7:Due date: 04/12/12, by 11:00 am.Problem # 1:The crude oil with temperature-independent physical properties is in fully developed laminarflow between two flat surfaces placed a distance 2B apart. For z < 0 the fluid is uniform at T =T1
University of Texas - PGE - 322K
Please read the following parts in the textbook (Bird et al, 2nd edition)1. Review of mathematics: (to be completed within two weeks from the date thisassignment posted)Appendix A2. Chapter 1 : the following sections (to be completed by 01/28/12)- 1.