lab 3: relative geologic time and stratigraphic

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1 LAB 3: RELATIVE GEOLOGIC TIME AND STRATIGRAPHIC INTERPRETATIONS PART I: RELATIVE TIME AND STRATIGRAPHY INTRODUCTION EXERCISE 3.1. Identifying Unconformities In Figure 3.2, an unconformity surface has been marked with a dark wiggly line. The specific type of unconformity is different depending on where along the wiggly line you look. Find examples of the three types of unconformities in Figure 3.2 and draw them in the labeled boxes. Include the rock textures (patterns) as they appear in the geological cross-section. Figure 3.2: Geological cross-section.

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Page 1: LAB 3: RELATIVE GEOLOGIC TIME AND STRATIGRAPHIC

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LAB3:RELATIVEGEOLOGICTIMEANDSTRATIGRAPHICINTERPRETATIONSPARTI:RELATIVETIMEANDSTRATIGRAPHYINTRODUCTION EXERCISE3.1.IdentifyingUnconformitiesInFigure3.2,anunconformitysurfacehasbeenmarkedwithadarkwigglyline.Thespecifictypeofunconformityisdifferentdependingonwherealongthewigglylineyoulook.FindexamplesofthethreetypesofunconformitiesinFigure3.2anddrawtheminthelabeledboxes.Includetherocktextures(patterns)astheyappearinthegeologicalcross-section.

Figure3.2:Geologicalcross-section.

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EXERCISE3.2.ReconstructingRelativeGeologicalTime

Figure3.3isageologiccross-sectionwhereeachrockunitisassignedaletterasalabel.UsethelabelsinFigure3.3andthestratigraphicprinciplestoanswerthequestionsthatfollow.

Allrocksaresedimentaryexceptforthefollowing:

• H:metamorphic• PandS:intrusiveigneousrocks

Figure3.3:Geologicalcross-section.Thespacebelowisprovidedforyoutomakenotes.

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1. Whichistheoldestgeologicevent?____________________________________________________

2. WhichgeologiceventsaredefinitelyolderthantheintrusionS?____________________________

3. WhatstratigraphicprincipleisusedtodateFaultBontherightsideofthefigure?

_________________________________________________________________________________

4. Whichpairsofrocklayersdefineunconformities?________________________________________Tohelpyouwithquestion6,itmaybeusefultomarkthelocationofeachoftheseonyourdrawingbymakingthesecontactsthicker,orbyusingacolouredpenciltohighlighttheirlocations.

5. Whichisthemostrecent(youngest)geologicaleventinthecrosssectionabove?________________________________________________________________________________

6. Placetherockunitsandthefaults(usingthelettersAandB)inorderrangingfromtheoldesttothe

youngestbyplacingthecorrespondinglettersintothespacesbelow.

(Oldest)____,____,____,____,____,____,____,____,____,____,____,____,_____,_____(Youngest)

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PARTII:INTERPRETINGSTRATIGRAPHYINASTRATIGRAPHICLOGEXERCISE3.3–InterpretingStratigraphicLogsTables3.2and3.3summarizestratigraphiclogsfromtwodifferentlocations.Usethefollowinginstructionstointerpretandcompleteeachlog.Note:TheonlineLabManualincludesanexampleofwhatacompletedlogmightlooklike.

1. IdentifythedepositionalenvironmentbyinterpretingthewrittenfaciesdescriptionanddrawnstratigraphiccolumnusingtheinformationfromLab2.Writethenameoftheenvironmentnexttothelogsketch.

2. Startingatthebottomofthelog,decidewhetherthetransitionfromonefaciestothefaciesaboveitrepresentsachangetoadeeperwaterfacies(transgression)orashallowerwaterfacies(regression).Writethecorrespondingchange(TorR)intheboxonthehorizontallineseparatingthetwofacies.

3. Intheright-handcolumn,plotthefaciesaccordingitslocationbyshadingthecorrectdot.Forexample,ifanenvironmentisabeach,shadethedotunder"Beach."Therearealsodotsforintermediateenvironments.Ifanenvironmenthasdeeperwaterthan"Beach,"butshallowerthan"Shelf,"youwouldshadethedotbetweenthosetwoenvironments.Rememberthattheprogressionfromfinefar-offshoresedimentstocoarsecoastalsedimentsmaynotbesmooth.Onceyou'veshadedthecorrectdots,connectthedotsusingstraightlinestocreateasealevelcurveliketheoneshowninFigure3.9.

4. Indicateperiodsoftransgressionorregressionbyplacingarrowsonthestraightlinespointingleft(transgression)orright(regression).(SeeFigure3.10intheonlineLabManual.)

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Table3.2:Siliclasticdominatedsystem.FaciesDescription

Strat.Log

Environment RelativeSeaLevelHighLow(Transgressions) (Regressions)OceanTerrestrialBasinShelfBeachDistalProximal

Hummockysequences;silt;lowanglecrossbedsandripples;abundantmarinefossils

¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ Shadethecorrectdotforeachenvironment,thenconnecttheshadeddotstodrawthesea-levelcurve. ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢

Gravelsdowncuttinglaminatedsilts,overlainbysands,thensilts,plantfragments

Darkorganicsilt,mud,stormwashsandlayers,Cruziana

Quartzsst.;abundantripples,Skolithos

Hummockysequences;sandandsiltwithalayerofgravelnearthebase

Qtzsst.;gentlydippingparallellaminations,shells,wooddebris.

¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢

*Startingfromthebottomofthestratigraphiccolumn,markintheboxnexttoeachboundarylinebetweenfacieswhetherthefacieschange,movingupwardsinthecolumn,representsthatsealevelistransgressing(T)orregressing(R).

Trans.orRegress.T/R*

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Table3.3:Carbonatedominatedsystem.FaciesDescription

Strat.Log

Environment RelativeSeaLevelHighLowTransgressionsRegressionsOceanTerrestrialBasinShelfBeachDistalProximal

Light-grey,unbeddedbiolithite;debrisflowsandslumps

Shadethecorrectdotforeachenvironment,thenconnecttheshadeddotstodrawthesea-levelcurve. ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢ ¢

Medium-beddedmicritewithlimesandlenses;clamcoquina,patchreefs

Algallaminateddolomite;mudcracks.,gypsum

Grey-greenhummockybedsofpackedbiomicriteinterbedddwithveryburrowedbiomicrite

Thinlylaminatedblackmicrites

*Startingfromthebottomofthestratigraphiccolumn,markintheboxnexttoeachboundarylinebetweenfacieswhetherthefacieschange,movingupwardsinthecolumn,representsthatsealevelistransgressing(T)orregressing(R).

Trans.orRegress.

T/R*