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Maryland - FINANCE - BMGT343
Chapter 4Mutual Funds andOther InvestmentCompaniesMcGraw-Hill/Irwin4-1Copyright 2010 by The McGraw-Hill Companies, Inc. All rights reserved.Services of Investment CompaniesDiversificationb.d.Low cost, instant diversificationProfessional manage
Maryland - FINANCE - BMGT343
Chapter 5Risk and Return:Past and PrologueMcGraw-Hill/Irwin5-1Copyright 2010 by The McGraw-Hill Companies, Inc. All rights reserved.5.1 Rates of Return5-2Measuring Ex-Post (Past) ReturnsOne period investment: regardless of the length of theperio
Maryland - INFO - BMGT302
CHAPTER 0AN OVERVIEW OF COMPUTERSAND PROGRAMMING1BMGT 302Business Application ProgrammingBy Peng HuangR.H. Smith School of Business, University of MarylandUNDERSTANDING COMPUTER SYSTEMSComputer systemCombination of all the components required to
Maryland - INFO - BMGT302
CHAPTER 1AN INTRODUCTION TO VISUALBASIC 20101BMGT 302Business Application ProgrammingBy Peng HuangR.H. Smith School of Business, University of MarylandA LITTLE HISTORYVisual Basic is evolved from BASICBeginners All-purpose Symbolic Instruction C
Maryland - INFO - BMGT302
CHAPTER 2DESIGNING USER INTERFACE1BMGT 302Business Application ProgrammingBy Peng HuangR.H. Smith School of Business, University of MarylandPLANNING AN APPLICATIONPlan the application before creating the userinterface Work jointly with the user
Maryland - INFO - BMGT302
CHAPTER 3VARIABLES AND CALCULATIONS1BMGT 302Business Application ProgrammingBy Peng HuangR.H. Smith School of Business, University of MarylandINTERNAL MEMORYInternal memory: a component inside acomputer comprised of memory locations Each memory
Maryland - INFO - BMGT302
CHAPTER 4MAKING DECISIONS1BMGT 302Business Application ProgrammingBy Peng HuangR.H. Smith School of Business, University of MarylandTHE SELECTION STRUCTURESelection structure (or decision structure):A decision need to be made based on the outcome
Marshall - GLY - 421
ERSC 4012El-Shazly, A. K., 1997.HOMEWORK PROBLEM # 1FIELD TRIP to BIDBIDThe purpose of this field trip is to examine some of the metamorphic rocks that occur atthe base of the ophiolite (known as the metamorphic sole), and to figure out thecondition
Marshall - GLY - 421
1GLY 421: Petrology of the Blue Ridge Province, VASpring, 2010Preparation for the trip:Read the sections in your textbook on1- Igneous structures (Chapter 4)2- Go over the chapter on the classification of igneous rocks.3- Go over the nomenclature o
Marshall - GLY - 421
GLY 421: Igneous & Metamorphic PetrologyEl-Shazly, 20041Classification of Igneous RocksThe classification of igneous rocks is not easy. This is simply because igneous rocksrepresent a continuum in nature (whether mineralogically or chemically), makin
Marshall - GLY - 421
GLY 421: Igneous & Metamorphic PetrologyEl-Shazly, A. K., 20041Magmatic DifferentiationDifferentiation is the process by which magmas evolve to give rise to a variety ofmagmas and rock types (that have different compositions). Therefore, certain phys
Marshall - GLY - 421
1METAMORPHIC FACIESMetamorphic Zones and IsogradsOne of the main objectives of studying metamorphic rocks is to identify the directions ofincrease or decrease in metamorphic grade within an area, as a first step towardsunderstanding the tectonic hist
Marshall - GLY - 421
1Estimation of P & T: ThermobarometryA- GeothermometryI- The petrogenetic grid approach:This approach relies on calculating petrogenetic grids for specific chemical systems,determining the P-T locations of the different metamorphic reactions, and est
Marshall - GLY - 421
GLY 441: Igneous & Metamorphic PetrologyEl-Shazly, A. K., 2004Granites and Granitic Rocks(Reading: Winter p. 343 -358)General features of Granitoids: Occurrence and Abundance Field relations Batholiths, stocks, and cupolas. Ptygmatic folds. Encla
Marshall - GLY - 421
GLY 421: Igneous & Metamorphic PetrologyEl-Shazly, 20041I- IntroductionDefinitions:Petrology: Is the study of rocks. Igneous petrology is that branch of petrology dealingwith the study of rocks that were originally molten (i.e. which formed from mag
Marshall - GLY - 421
PART II: METAMORPHIC PETROLOGYINTRODUCTIONWhat is metamorphism?"Metamorphism is the mineralogical and/or textural adjustments that take place in arock in response to a new set of physicochemical conditions different from the onesunder which the rock
Marshall - GLY - 421
1Equilibrium vs. non-equilibrium in metamorphic rocksReaction KineticsReaction kinetics refers to the rates at which reactions take place. For metamorphicreactions, this type of study is very difficult. Most metamorphic reactions are veryslow or slug
Marshall - GLY - 421
GLY 421: Igneous & Metamorphic PetrologyEl-Shazly, 20041Magmas and LavasDefinitions:Magma: a mixture of a melt (predominantly silicate) crystals volatiles which occursat depths and has the ability to migrate to shallower levels where it either cryst
Marshall - GLY - 421
1Metamorphism and TectonicsDefinitions:Steady state geotherm: Is that curve defining the change in T as a function of depth in anarea that is not experiencing any tectonic activity such as a stable shield or continentalinterior.Transient geotherm: I
Marshall - GLY - 421
1Lab 7Acidic Volcanic and Plutonic RocksAs you are aware, "volcanic" (s.l.) rocks are either lava flows or pyroclastics. Whereaslava flows have a wide range in compositions (from SiO 2 undersaturated rocks asleucitophyres and phonolites, through basa
Marshall - GLY - 421
Lab 6Miscellaneous volcanic and plutonic SiO2 undersaturated rocksIn this lab, you will examine a variety of alkalic and/or SiO 2 undersaturated rocks, suchas foid syenites, phonolites, Nephelenites, leucitites, leucitophyres, carbonatites, andkimberl
Marshall - GLY - 421
1Lab 9Part A: Metabasalts from KaramutsenThe Karamutsen Group of NE Vancouver Island, western Canada, consists ofsubmarine basaltic rocks (tuffs, massive flows and pillow lavas). These rocksunderwent low -grade burial metamorphism prior to the intrus
Marshall - GLY - 421
1Lab 10Metabasalts from KaramutsenThe Karamutsen Group of NE Vancouver Island, western Canada, consists ofsubmarine basaltic rocks (tuffs, massive flows and pillow lavas). These rocksunderwent low -grade burial metamorphism prior to the intrusion of
Marshall - GLY - 421
1Lab 12High Pressure Metamorphic Rocks from Saih Hatat, Oman(mostly mafics)In this section, you will examine samples that represent a progressive metamorphicsequence from Region III, Saih Hatat, NE Oman (Fig. 2). For this lab, all you have to dois e
Marshall - GLY - 421
1Lab 1Optical properties of common igneous and metamorphic mineralsIntroduction:Minerals in igneous and metamorphic rocks are either:1- Essential minerals: these are the minerals whose presence, absence and abundanceinfluence the rock name. They mus
Marshall - GLY - 421
1Lab 2Description of Igneous Rock Samples in Hand Specimen and ThinSectionA- Field description:1- Location2- Structures3- Color and color index (C.I.; see below)4- Average grain size (overall):Phaneritic: very coarse (> 1cm), coarse (5mm 1cm), me
Marshall - GLY - 421
1Lab 3Ultramafic and Mafic plutonic rocksIn this lab, you will learn how distinguish between olivine, clinopyroxene andorthopyroxene in hand specimen, and how to identify them quickly and efficiently inthin section. For all samples with a hand specim
Marshall - GLY - 421
1Lab 4Dolerites and basaltsPart ADoleritesDolerites are fine-grained gabbroic rocks that occur as intrusives. As such, dolerites canbe called "microgabbros". Another name for a dolerite is "diabase", which is commonlyused in the US, although many B
Marshall - GLY - 421
1Lab 5Andesites, Latites, Trachytes, Dacites and RhyodacitesIn this lab, we will examine volcanic rocks that are more "differentiated" than basalts.The main objective of this lab is to train you to classify these rocks, and to be able totell them apa
Marshall - GLY - 421
1ERSC 4011El-Shazly, A. K., 1995Lab 8Samples from the Semail OphioliteAs you are aware, the Semail ophiolite consists of(1) Tectonized harzburgites with pods and lenses of dunite,(2) Layered gabbros(3) Isotropic gabbros(4) Sheeted dykes(5) Pillo
Marshall - GLY - 421
Geol 331: Igneous & Metamorphic PetrologyEl-Shazly, 20021Lab 11Metamorphism of PelitesIn this lab, you will examine thin sections representing the metamorphism of peliticrocks under two different facies series (in two separate problems) spanning the
Marshall - GLY - 421
Hand-Specimen Description of Metamorphic RocksMineralogy:(a) Essential minerals(b) Accessory minerals(c) Secondary minerals(d) Index mineralsTextures:(a) Grain size(b) General texture(c) Special texturesFacies (metamorphic grade):Protolith:Roc
Marshall - GLY - 421
1ERSC 4011El-Shazly, A. K., 1996Outcrops of the Ophiolite Suite along route 23In this field trip we will examine the different rock types of the Semail ophioliteexposed along route 23. The main objective of this field trip is to train you to recogniz
Marshall - GLY - 421
1GLY 421El-Shazly, A. K., 2004Crystallization of Magmas: Crystal liquid equilibriaa- Equilibrium and the phase ruleDefinitions:Equilibrium: A system is said to be in equilibrium if there is no observed change withinit over time. At equilibrium, the
Marshall - GLY - 421
1P-T-time pathsDefinition:A P-T-time path is a loop or curve connecting all P and T points to which a rock hasbeen subjected from the beginning of its metamorphic history until the time of itsexhumation (exposure) at the surface.Each rock or hand sa
Marshall - GLY - 421
1METAMORPHIC REACTIONSSince we have decided to use an equilibrium approach for studying metamorphicrocks, the law of mass action can be applied to any metamorphic reaction. This meansthat every metamorphic reaction will have an equilibrium constant.T
Marshall - GLY - 421
A- Hand Specimen DescriptionSample #: UTM-1Color and color index: LeucocraticC.I.: 12Average grain size (overall): Coarse grained.General texture: Holocrystalline; equigranular hypidiomorphicMineralogy:(a) Essential Minerals:K-feldspar (35%), Plag
Marshall - GLY - 421
1ERSC 4012El-Shazly, February, 12FIELD TRIP TO SAIH HATAT&HOMEWORK PROBLEM # 5HIGH PRESSURE METAMORPHISM IN SAIH HATATThis field trip is aimed at examining some of the high pressure, low temperaturemetamorphic rocks which occur in the Saih Hatat a
Marshall - GLY - 421
1The Skaergaard IntrusionA natural lab for studying closed system fractionation?The Skaergaard intrusion is a large 2.5 km - thick intrusion of tholeiitic magma intoPrecambrian quartzofeldspathic gneisses in eastern Greenland. It was emplaced in theE
Marshall - GLY - 421
Geol 331: Igneous & Metamorphic PetrologyMcCutcheon & El-Shazly, 2002Field trip to the St. Francois Mountains, MissouriMarch/ April every other yearPreparation for the trip:Read the sections in your textbook on1- Calderas, cauldron subsidence, ring
Marshall - GLY - 421
Geology 421: Petrology(Igneous & Metamorphic Petrology)Credit hours: 4 unitsInstructor: Aley El-Din El-ShazlyOffice: 131 Science Buildinge-mail: elshazly@marshall.eduTel: 696-6756Lectures: TR 11 12:15 a.m., Science 125Lab: T: 1:00 2:50 p.m., Scien
Marshall - GLY - 421
1Metamorphism and TectonicsDefinitions:Steady state geotherm: Is that curve defining the change in T as a function of depth in anarea that is not experiencing any tectonic activity such as a stable shield or continentalinterior.Transient geotherm: I
Marshall - GLY - 421
1GLY 421: Igneous & Metamorphic PetrologyEl-Shazly, A. K., 2004Ternary Phase DiagramsGeneral principles:Construction of ternary phase diagrams: Ternary phase diagrams are constructed byprojecting the liquidus surfaces of a three dimensional diagram
Marshall - GLY - 421
1Compositional phase diagramsUses of compositional phase diagrams:(i) They show the relationship between the bulk composition of a rock and its mineralassemblage.(ii) They help illustrate the stable mineral assemblage at a specified P and T(iii) The
Marshall - GLY - 421
1Metamorphic TexturesTexture: Is a term that describes the size, shape and orientation of the grains constitutinga rock, as well as the relationship between these grains.Elements of metamorphic textures:1- Crystal size:<0.1 mm0.1-1mm1-5 mm5-10mm
Marshall - GLY - 421
1The Use of Trace Elements in Igneous PetrologyIntroduction:Trace elements are those which occur in very low concentrations in common rocks(usually < 0.1 % by weight). Their concentrations are therefore commonly expressed inparts per million (ppm; 1
Marshall - CHM - 218H
Carbonyl Compounds Homework KeyDraw the structures of the following compounds.OOformic acidethyl acetate C H C3HCO HO CH2 CH3Opentanoic acidisopropyl pentanoateC H 3C H2C H 2C H 2C O HC H3OOCH3O CHC H 3C H 2C H 2C H 2 CCH33-methylhexan
Marshall - CHM - 218H
Carbonyl Compounds Homework KeyDraw the structures of the following compounds.OOformic acidethyl acetate C H C3HCO HO CH2 CH3Opentanoic acidisopropyl pentanoateC H 3C H2C H 2C H 2C O HC H3OOCH3O CHC H 3C H 2C H 2C H 2 CCH33-methylhexan
Texas State - ACC - 3313
Chapter1:IntermediateAccounting06/02/201214:18:00Fin.acctheprocessthatculminatesintheprepoffin.Reportsontheenterprisefor usebybothinternalandexternalparties.Managementactoverseeingoperations4financialstatements:1. balancesheet2.Incomestatement3.Stat
Texas State - ACC - 3313
Intermediate AccountingIntermediateChapter 1FinancialAccountingandAccountingStandardsLearning ObjectivesLearning2IdentifythemajorfinancialstatementsandothermeansoffinancialreportingExplainhowaccountingassistsintheefficientuseofscarceresourcesDes
Texas State - ACC - 3313
CHAPTER 7SolutionsCASH AND RECEIVABLESChapter 7, SE 1.1.2.3.4.c (also could be a)abdChapter 7, SE 2.Net SalesReceivable Turnover ==Average Accounts Receivable$720,000$90,000(=$720,000$80,000$70,000=) 29.0 times365 daysDays' Sale
Texas State - ACC - 3313
Intermediate AccountingIntermediateChapter 1FinancialAccountingandAccountingStandardsLearning ObjectivesLearning2IdentifythemajorfinancialstatementsandothermeansoffinancialreportingExplainhowaccountingassistsintheefficientuseofscarceresourcesDes
Texas State - ACC - 3313
Intermediate AccountingIntermediateChapter 2ConceptualFrameworkUnderlyingFinancialAccountingLearning ObjectivesLearning2DescribetheusefulnessofaconceptualframeworkDescribetheFASBseffortstoconstructaconceptualframeworkUnderstandtheobjectiveoffina
Texas State - ACC - 3313
IntermediateAccountingChapter3TheAccountingInformationSystemLearning ObjectivesLearning2UnderstandbasicaccountingterminologyExplaindoubleentryrulesIdentifystepsintheaccountingcycleRecordtransactionsinjournals,posttoledgeraccounts,andprepareatri
Texas State - ACC - 3313
IntermediateAccountingChapter4IncomeStatementandRelatedInformationLearning ObjectivesLearningUnderstandtheusesandlimitationsofanincomestatement Prepareasinglestepincomestatement Prepareamultiplestepincomestatement Explainhowtoreportirregularitems
Texas State - ACC - 3313
Intermediate AccountingIntermediateChapter 5BalanceSheetandStatementofCashFlowsLearning ObjectivesLearning2ExplaintheusesandlimitationsofabalancesheetIdentifythemajorclassificationsofthebalancesheetPrepareaclassifiedbalancesheetusingthereportandt
Texas State - ACC - 3313
IntermediateAccountingChapter7CashandReceivablesLearning ObjectivesLearning2IdentifyitemsconsideredcashIndicatehowtoreportcashandrelateditemsDefinereceivablesandidentifythedifferenttypesofreceivablesExplainaccountingissuesrelatedtorecognitionofac
Texas State - ACC - 3313
Intermediate AccountingIntermediateChapter 9Inventories:AdditionalValuationIssuesLearning ObjectivesLearning2DescribeandapplythelowerofcostofmarketruleExplainwhencompaniesvalueinventoriesatnetrealizablevalueExplainwhencompaniesusetherelativesales
Texas State - ACC - 3313
IntermediateAccountingChapter10AcquisitionandDispositionofProperty,Plant,andEquipmentLearning ObjectivesLearning2Describeproperty,plant,andequipmentIdentifythecoststoincludeininitialvaluationofproperty,plant,andequipmentDescribetheaccountingprob
Texas State - ACC - 3313
IntermediateAccountingChapter11Depreciation,Impairments,andDepletionLearning ObjectivesLearningDescribetheconceptofdepreciationIdentifythefactorsinvolvedinthedepreciationprocessCompareactivity,straightline,anddecreasingchargemethodsofdepreciation
Texas State - FIN - 3313
Dr. Sudhakar RajuFN 3000ASSIGNMENT QUESTIONS FOR CHAPTER 4 (Time Value of Money)1. First City Bank pays 7 percent simple interest on its savings account balances, whereasSecond City Bank pays 7 percent interest compounded annually. If you made a $6,00