Exam 2

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Geology

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What contents of field notes are required to draw lithostratigraphic columns

<p></p>
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<p>What lithology is this?</p><p></p>

What lithology is this?

Conglomerate

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<p>What lithology is this?</p><p></p>

What lithology is this?

Sandstone

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<p>What lithology is this?</p>

What lithology is this?

Limestone

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<p>What lithology is this?</p>

What lithology is this?

Dolomite

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<p>What lithology is this?</p>

What lithology is this?

Shale

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Lithostratigraphic Hierarchy

  • Super group: largest unit, made of two or more groups or formations that share lithological characteristics

  • Group: mode of two or more formations with shared lithological features

  • Formation: the primary and most essential unit, defined by its lithological properties and map ability.

  • Member: subdivision of formation, with distinct characteristics but not mappable at scale of formation

  • Bed: smallest unit, representing distinct depositional layer

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Taxon-range Zone

Single taxon

<p>Single taxon</p>
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Concurrent-range Zone

Uses two taxa

<p>Uses two taxa</p>
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Assemblage Zone

knowt flashcard image
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What does the Caliper sensor measure?

The size of the drilled borehole

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Electrical Sensors measure?

Detects porewater amount, permeability, and ionic concentration of sediment and porewater

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Gamma-ray sensors measure?

Measure the amount and type of radioactive elements (U, Th, K) in sediment

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What is drilling mud composed of?

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Functions of Drilling Fluids

  • Provide hydrostatic pressure to control the well

  • Create a seal between borehole and formation

  • Remove rock cutting from the well

  • Lubricate and cool the drill string

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Types of Drilling Fluids

  • water-based muds

  • oil-based muds

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Properties of Drilling Fluids

  • mud weight

  • viscosity

  • pH

  • Fluid Loss

  • Salinity

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Composition of Drilling Muds

bentonite clay to increase viscosity and suspend cuttings, and barite to add weight.

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Bed strength/induration/cemented

Caliper measures this.

<p>Caliper measures this.</p><p></p>
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Caliper Measurements

  • on gauge: well consolidated formations, non-permeable formations

    • massive sandstones

    • calcareous shales

  • Larger than bit size: Formation soluble in drilling mud or formations weak and cave in.

    • Salt formations drilled with fresh water

    • unconsolidated sands, gravels, and brittle shales

  • Smaller than bit size: formations swell and flow into borehole or development of mudcake for porous and permeable formations

    • swelling shales

    • porous, permeable sand stones

<ul><li><p>on gauge: well consolidated formations, non-permeable formations</p><ul><li><p>massive sandstones</p></li><li><p>calcareous shales</p></li></ul></li><li><p>Larger than bit size: Formation soluble in drilling mud or formations weak and cave in.</p><ul><li><p>Salt formations drilled with fresh water</p></li><li><p>unconsolidated sands, gravels, and brittle shales </p></li></ul></li><li><p>Smaller than bit size: formations swell and flow into borehole or development of mudcake for porous and permeable formations</p><ul><li><p>swelling shales</p></li><li><p>porous, permeable sand stones</p></li></ul></li></ul><p></p>
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<p><span><span>Spontaneous Potential (SP) Logs</span></span></p>

Spontaneous Potential (SP) Logs

  • measures natural electric potential

  • permeable formation, Low SP

  • Impermeable= higher SP

<ul><li><p>measures natural electric potential</p></li><li><p>permeable formation, Low SP</p></li><li><p>Impermeable= higher SP</p></li></ul><p></p>
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Resistivity Logs

  • is function of permeability, porosity and pore fluid salinity in rock

  • Frequently used to identify lithology that varies based on permeability

    • High Resistivity=little porewater

    • Low resistivity =more porewater

Remember, the more ionic charge (saline) in sediment (cations on clays or NaCl in porewaters), the greater the electrical conductance and less resistivity

<ul><li><p><span style="color: rgb(0, 0, 0);">is function of permeability, porosity and pore fluid salinity in rock</span></p></li><li><p><span style="color: rgb(0, 0, 0);"><span>Frequently used to identify lithology that varies based on permeability</span></span></p><ul><li><p><span style="color: rgb(0, 0, 0);"><span>High Resistivity=little porewater</span></span></p></li><li><p><span style="color: rgb(0, 0, 0);"><span>Low resistivity =more porewater</span></span></p></li></ul></li></ul><p></p><p>Remember, <strong>the more ionic charge (saline)</strong> in sediment (cations on clays or NaCl in porewaters), the greater the electrical conductance and <strong>less resistivity</strong></p>
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Gamma Ray Logs

  • Shales have high gamma radioactivity

Lithology from lowest to highest gamma radiation

Limestone: 5-10

Dolomite: 10-20

Sandstone: 10-30

Shale: 80-140

<ul><li><p>Shales have high gamma radioactivity</p></li></ul><p>Lithology from lowest to highest gamma radiation</p><p>Limestone: 5-10</p><p>Dolomite: 10-20</p><p>Sandstone: 10-30</p><p>Shale: 80-140</p><p></p>
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Gamma Ray Logs Interpretations

<p></p><p></p>
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Cylindrical GR

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  • Even block with sharp top and base

    • Eolian

    • Braided Fluvial

    • distributary channel-fill

    • submarine-canyon-fill

    • carbonate-shelf-margin

      • evaporite fill or basin

<ul><li><p>Even block with sharp top and base</p><ul><li><p>Eolian</p></li><li><p>Braided Fluvial</p></li><li><p>distributary channel-fill</p></li><li><p>submarine-canyon-fill</p></li><li><p>carbonate-shelf-margin</p><ul><li><p>evaporite fill or basin</p></li></ul></li></ul></li></ul><p></p>
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Funnel GR

  • Coarse up and sharp top:

    • crevasse splay

    • river mouth bar

    • delta front

    • shoreface

    • submarine fan lobe

    • change from clastic to carbonates

<ul><li><p>Coarse up and sharp top:</p><ul><li><p>crevasse splay</p></li><li><p>river mouth bar</p></li><li><p>delta front</p></li><li><p>shoreface</p></li><li><p>submarine fan lobe</p></li><li><p>change from clastic to carbonates</p></li></ul></li></ul><p></p>
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Bell GR

Fine up and sharp base:

  • fluvial point bar

  • tidal point par

  • deep tidal channel

  • tidal flat

  • transgressive shelf

<p>Fine up and sharp base:</p><ul><li><p>fluvial point bar</p></li><li><p>tidal point par</p></li><li><p>deep tidal channel</p></li><li><p>tidal flat</p></li><li><p>transgressive shelf</p></li></ul><p></p>
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Symmetrical GR

Prograding and retrograding

  • reworked offshore bar, regressive to transgressive shore face delta

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<p>Serrated GR</p>

Serrated GR

Saw teeth

  • fluvial floodplain

  • storm dominated shelf

  • distal deep-marine slope

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Dotted contact

Diffuse/gradual

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Sharp Contact

Straight Line

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Angular Unconformity

Tilted or folded, with new horizontal layer on top

<p>Tilted or folded, with new horizontal layer on top</p>
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Disconformity

Clear erosion between sedimentary layers

<p>Clear erosion between sedimentary layers</p>
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Nonconformity

Where sedimentary rock is deposited on top of igneous rock

<p>Where sedimentary rock is deposited on top of igneous rock</p>
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Paraconformity

Similar to a disconformity, this is a gap between parallel rock layers. The key difference is that there is no obvious erosional surface or discolored contact; it is a gap where beds are parallel and little apparent erosion has occurred. 

<p><span><span>Similar to a disconformity, this is a gap between parallel rock layers. The key difference is that there is no obvious erosional surface or discolored contact; it is a gap where beds are parallel and little apparent erosion has occurred.&nbsp;</span></span></p>
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Sandstone on shale

Sharp Contact

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Sandstone on Conglomerate

Diffuse contact

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Bed strength/induration/cemented

Use Caliper

On gauge: Well consolidated

Larger than bit: Formation weak and cave in

Smaller than bit: Formations swelling or development of mud cake for porous and permeable formations

<p>Use Caliper</p><p>On gauge: Well consolidated</p><p>Larger than bit: Formation weak and cave in</p><p>Smaller than bit: Formations swelling or development of mud cake for porous and permeable formations</p>
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Permeable vs. impermeable beds

Caliper: non permeable formations are on guage, permeable form mudcakes and show smaller than bit size

Spontaneous Potential (SP): permeable= low SP

impermeable= high SP

Resistivity Logs: HLow resistivity =more porewater (permeable)

Low resistivity=little porewater (impermeable)


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Swelling lithologies

Caliper: smaller than bit size= swelling

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High ionic strength pore fluids

Resistivity Logs: the more ionic charge in the sediment, the less resistivity

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Fining/coarsening upward sequences

Gamma Ray Log

Gamma ray logs infer grain size (and so subsequently inferred depositional energy)

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Gamma Ray Logs: Shale

  • Value: 80-140

  • Shale has high gamma radioactive Response

<ul><li><p>Value: 80-140</p></li><li><p>Shale has high gamma radioactive Response</p></li></ul><p></p>
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Caliper Log: Shale

  • most shales are on gauge

  • Larger than bit= brittle shales (caving)

  • Smaller than bit= swelling shales (sloughing)

<ul><li><p>most shales are on gauge</p></li><li><p>Larger than bit= brittle shales (caving)</p></li><li><p>Smaller than bit= swelling shales (sloughing)</p></li></ul><p></p>
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Spontaneous Potential (SP) Log: Shale

Impermeable Shale= Higher SP Value

Give an indication of shaliness (maximum negative deflection is clean porous, permeable sand; minimum/low SP is shale or cemented limestone)

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Resistivity Logs: Shale

  • Low resistivity

  • Deep and shallow are the same

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Caliper Logs: Sandstone

  • On gauge: Impermeable sandstone

  • Smaller than bit size: Permeable sandstone

  • Larger than bit size: unconsolidated sands

<ul><li><p>On gauge: Impermeable sandstone</p></li><li><p>Smaller than bit size: Permeable sandstone</p></li><li><p>Larger than bit size: unconsolidated sands</p></li></ul><p></p>
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Spontaneous Potential (SP) Logs: Sandstone

Low SP, because sand is permeable

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Resistivity Logs: Sandstone

Tight Sandstone: Higher than shale, higher than porous sandstone

Porous Sandstone: Higher than shale, lower than tight sandstone

<p>Tight Sandstone: Higher than shale, higher than porous sandstone</p><p>Porous Sandstone:&nbsp;Higher than shale, lower than tight sandstone</p>
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Gamma Ray Log: Sandstone

Low gamma ray value, but higher than limestone

Acts as representation of grainsize

<p>Low gamma ray value, but higher than limestone</p><p>Acts as representation of grainsize</p><p></p>
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Gamma Ray Log: Limestone

Very low

Lower than sandstone and shale

<p>Very low</p><p>Lower than sandstone and shale</p>
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Caliper Log: Limestone

Probably on gauge

<p>Probably on gauge</p>
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Spontaneous Potential (SP) Logs

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