petro petro lo lo gi gi 2 SKS teori 2 SKS teori 1 SKS praktikum 1 SKS praktikum by: by: hill. gendoet hartono hill. gendoet hartono Semester 2, 2008-2009 Semester 2, 2008-2009 Senin, jam 09.50 – 10.40 Senin, jam 09.50 – 10.40 jam 10.45 – 11.35 jam 10.45 – 11.35
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
petropetrolologigi2 SKS teori2 SKS teori1 SKS praktikum1 SKS praktikum
by:by:hill. gendoet hartonohill. gendoet hartono
Semester 2, 2008-2009Semester 2, 2008-2009
Senin, jam 09.50 – 10.40Senin, jam 09.50 – 10.40 jam 10.45 – 11.35jam 10.45 – 11.35
Clastic Rocks - Hand SpecimensClastic Rocks - Hand Specimens
Particle size is used to distinguish among Particle size is used to distinguish among the various types of detrital rocksthe various types of detrital rocks
MudrocksMudrocks: grains less than .06 mm: grains less than .06 mm1. Mud1. Mud: small particles easily kept in suspension: small particles easily kept in suspension Settles only in quiet waterSettles only in quiet water Rock types include Rock types include ShaleShale: m: mud-sized particles ud-sized particles
<.004 mm deposited in thin bedding layers called <.004 mm deposited in thin bedding layers called laminaelaminae
The most common sedimentary rockThe most common sedimentary rock
2. 2. Larger mudrock grains called Larger mudrock grains called siltssiltssilt-sized particles .004-.06 mmsilt-sized particles .004-.06 mm
Gritty grains can be feltGritty grains can be felt
SandstonesSandstonesMade of sand-sized particles .064 – 2 mm … Sand is Made of sand-sized particles .064 – 2 mm … Sand is
a size!a size!Forms in a variety of environmentsForms in a variety of environmentsSorting, angularity and composition of grains can Sorting, angularity and composition of grains can
be used to interpret the rock’s historybe used to interpret the rock’s historyQuartz is the predominant mineral (due to its Quartz is the predominant mineral (due to its
durable nature)durable nature)
Sandstone (note large number of quartz grains)Sandstone (note large number of quartz grains)
Photomicrograph of quartz rich sandstone (Arenite)Grains subangular to subrounded, sandstone is poorly sorted
Plagioclase grainPlagioclase grain
Classifying SandstonesClassifying Sandstones
Making thin sectionsMaking thin sections
Types of SandstoneTypes of Sandstone
Quartz Arenite >90% quartz grainsQuartz Arenite >90% quartz grains Beach and dune depositsBeach and dune deposits
Arkoses >25% feldspar, angular, poor sort.Arkoses >25% feldspar, angular, poor sort. Transform boundaries; exposed granitesTransform boundaries; exposed granites Any felsic rock eroded, not transported farAny felsic rock eroded, not transported far
Graywackes Quartz, feldspar, volcanicsGraywackes Quartz, feldspar, volcanics Port sorted, angularPort sorted, angular Erosion of Island ArcsErosion of Island Arcs Rift Valley Sediments Rift Valley Sediments
Coarse sediments are deposited in high Coarse sediments are deposited in high energy (fast water) environments such as energy (fast water) environments such as under breaking waves at the beach, or in under breaking waves at the beach, or in the beds of fast streams.the beds of fast streams.
Fine sediments are deposited in low Fine sediments are deposited in low energy environments, e.g. the slow water energy environments, e.g. the slow water of deep lagoons, the abyssal plain, etc.of deep lagoons, the abyssal plain, etc.
Outcrop of conglomerateOutcrop of conglomeratewith cobble-sized clasts with cobble-sized clasts interbedded with sandstoneinterbedded with sandstone
Conglomerates are fast-water sediments“High Energy”K.E. = 1/2mv2
In fast water, smaller sizes In fast water, smaller sizes swept awayswept away
Common chemical sedimentary rocksCommon chemical sedimentary rocksLimestoneLimestone
Most abundant chemical rockMost abundant chemical rockMade of the mineral calcite CaCOMade of the mineral calcite CaCO33
Marine biochemical limestones form Marine biochemical limestones form as coral reefs,as coral reefs, coquinacoquina (broken (broken shells), and shells), and chalk chalk (microscopic (microscopic organisms)organisms)
Inorganic limestones include Inorganic limestones include travertinetravertine (caves) and (caves) and oolitic oolitic limestonelimestone ( (BahamasBahamas))
Coquina Coquina
Fossiliferous limestoneFossiliferous limestoneNote shells and lime matrix
Chalk Outcrops in SE USA
Chalk Hand Specimen
Oolitic Limestone - Bahama Shoals
Oolitic Limestone - Hand Specimen
Ooids under microscopeInorganic Chemical SedimentsInorganic Chemical Sediments
Other chemical sedimentary rocksOther chemical sedimentary rocksChertChert
Made of microcrystalline quartzMade of microcrystalline quartz Usually deposited as siliceous ooze in deep Usually deposited as siliceous ooze in deep
oceans (can be diatomaceous)oceans (can be diatomaceous)
chertDiatomaceous chert
Other chemical sedimentary rocksOther chemical sedimentary rocks Dolostone (made of mineral Dolomite)Dolostone (made of mineral Dolomite) Like Calcite, but some Ca is replaced by MgLike Calcite, but some Ca is replaced by Mg
The Dolomites, sediments thrust up when the Alps formedThe Dolomites, sediments thrust up when the Alps formed
Chemical sedimentary rocksChemical sedimentary rocks
Common chemical sedimentary rocksCommon chemical sedimentary rocksCoalCoal
Different from other rocks because it Different from other rocks because it is composed of organic material is composed of organic material
Stages in coal formation (in order)Stages in coal formation (in order)1. Plant material1. Plant material2. Peat2. Peat3. Lignite3. Lignite4. Bituminous4. Bituminous
Stages in coal formationStages in coal formation
Sedimentary EnvironmentSedimentary Environment
Is the geographic setting where Is the geographic setting where sediment accumulatessediment accumulates
Determines nature of sediment that Determines nature of sediment that accumulates (grain size, shape, etc.)accumulates (grain size, shape, etc.)
6_56_5
Particles are large andirregular, and consist ofa variety of lithologies,including the leastresistant.
Particles are mid-sizedand of intermediatesphericity, and includeresistant and nonresistantlithologies.
Particles are small andnearly spherical, andconsist mainly of themost resistant lithologies,such as quartz.
Character of detrital sediments depends on time, distance, Character of detrital sediments depends on time, distance, and energy. For example, in streams:and energy. For example, in streams:
Types of sedimentary environmentsTypes of sedimentary environmentsTransitional (shoreline)Transitional (shoreline)
Tidal flat Sands w/ symmetrical ripplesTidal flat Sands w/ symmetrical ripplesLenses of tidal creek mudsLenses of tidal creek muds
Lagoons – including Bays behind Barrier Lagoons – including Bays behind Barrier Islands.Islands.Organic rich black muds and sandsOrganic rich black muds and sands
DeltasDeltasComplex, e.g. Sandstones w/ large Complex, e.g. Sandstones w/ large
foresets at seaward faceforesets at seaward face
A picture glossary of sedimentary environmentsTurbidite: underwater landslide = graded bedding
Sedimentary Sedimentary FaciesFaciesDifferent sediments accumulate Different sediments accumulate next to each other at same timenext to each other at same time
Each unit (called a Each unit (called a faciesfacies) possesses ) possesses a distinctive characteristics a distinctive characteristics reflecting the conditions in a reflecting the conditions in a particular environmentparticular environment
The merging of adjacent facies The merging of adjacent facies tends to be a gradual transitiontends to be a gradual transition
Nearshore sandsStillwater mudsAbyssal Ooze
Some facies in an oversimplified drawing
Sedimentary structuresSedimentary structuresTell us something about past Tell us something about past
environmentsenvironmentsTypes of sedimentary structuresTypes of sedimentary structures
Strata, or beds (most Strata, or beds (most characteristic of sedimentary characteristic of sedimentary rocks)rocks)-bedding planes that separate -bedding planes that separate strata caused by variation in strata caused by variation in depositiondeposition
Strata- Bedding PlanesStrata- Bedding Planes
Fine Scale Bedding- LamellaeFine Scale Bedding- Lamellae
Recognizable Sedimentary StructuresRecognizable Sedimentary Structures Types of sedimentary structures 1Types of sedimentary structures 1
Symmetric types formed in tidal areasSymmetric types formed in tidal areas
Cross Beds – Cross Beds – ripples in cross sectionripples in cross section
In cross section these look like lines In cross section these look like lines at an angle to the horizontal – “cross at an angle to the horizontal – “cross beds”beds”
Form determined by velocity and size Form determined by velocity and size of particles.of particles.
Slabs of eroding sandstone with ripple marks
Cross bedding in Sand Dune deposits
Sandstone deposited Sandstone deposited in ancient sand dunes in ancient sand dunes
Sand Dune? Look for Frosted GrainsNavaho Sandstone
Also good for right side upAlso good for right side up
Mud Cracks: clay layer shrinks during drying, curls upward; cracks fill next flood
Mudcracks indicate drying events. Geologists can determine if rocks overturned.
Sedimentary EnvironmentsSedimentary Environments
Sediments are formed in many different Sediments are formed in many different environmentsenvironments
Each have characteristic appearance Each have characteristic appearance today, features that allow them to be today, features that allow them to be recognized in the geologic recordrecognized in the geologic record
• Streams (includes big Rivers), with floodplains and levees, called fluviatile. The Point Bar Sequence is typical for meandering streams. Cutoffs generate Oxbow deposits.
High gradient streams with high sediment load are Braided.
• Lake deposits called lacustrine, generally still waters, often varved deposits if winters cold
Terms for Marine (i.e. Ocean) Environmentsand some characteristic sediment facies
AbyssalPlain
6_296_29River Direction of migration
of shoreline, and landwardshift of sedimentary facies
Shoreline attime B
Shoreline attime A
Time B
Time ASea levelrising
Depositedat time A
Depositedat time B
Shallowmarine
BeachRiver
Deepmarine
Deepmarine
Shallowmarine
Beach
Shallowmarine
Comparison of sediments deposited
Facies changes due to rising sea level - water getting deeper everywhere
REMEMBER: the facies follow the shoreline
Fossils: Evidence of past lifeFossils: Evidence of past life
By definition, fossils are the traces or By definition, fossils are the traces or remains of prehistoric life now preserved in remains of prehistoric life now preserved in rockrock
Fossils are generally found in sediment or Fossils are generally found in sediment or sedimentary rock (very rarely in sedimentary rock (very rarely in metamorphic or igneous rocks)metamorphic or igneous rocks)
Fossils: Evidence of past lifeFossils: Evidence of past life
Geologically fossils are important for Geologically fossils are important for several reasonsseveral reasons
Aid in interpretation of the geologic pastAid in interpretation of the geologic pastServe as important time and environment Serve as important time and environment
indicatorsindicatorsAllow for correlation of rocks from different Allow for correlation of rocks from different
placesplaces
3 Billion Year Old Algal Mounds (Stromatolites) Australia
CO2 inO2 out
Natural casts of Natural casts of shelled invertebrates in limestoneshelled invertebrates in limestone
Dinosaur footprint in mudstoneDinosaur footprint in mudstone
Dilophosaurus Jurassic Park Dennis Neary and Peter Dodson