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Sedimentary Rock Geology Lecture Series, From various sources By M. Nukman

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  • Sedimentary Rock

    Geology Lecture Series,

    From various sources

    By M. Nukman

  • Three Components

    Transportation

    Deposition

    Diagenesis

  • Transportation

    Sedimentary particle can be transported by sliding (longsoran) from a slope (energi gravitasi),

    It can be transported by the wind,

    It can be transported by water (river, ocean current)

    Gravitational within water (turbidite)

  • By water (transportation contd)

    Traction (touch the bottom, saltation)

    Density current (no traction, but more dense suspension, form a chaotic texture)

  • Deposition

    Sediment particle is deposited when the transportation energy is too low to bring those particles

    Type

    Suspension (flying out in water)

    Gravitational process (a denser particle will be faster to reach the bottom)

    Implication to sedimentary structure

  • Diagenetic

    Compaction due to overburden,which will reduce the pores

    A water filled the pores will precipitate,could form a new mineral within the pore

    Those new minerals joined the grains together cemented

  • Sedimentary Texture

    1. Grain Size

    = energi transportasi,

    see Wentworth scale

    2. Sortasi

    = keseragaman ukuran butir

    v.w. sorted-w.sorted-m.sorted-p.sorted

  • Wentworth ScaleName of

    ParticleSize Range Loose

    SedimentConsolidated

    Rock

    Boulder >256 mm Gravel Conglomerate or Breccia (depends on rounding)

    Cobble 64 - 256 mm Gravel

    Pebble 2 - 64 mm Gravel

    Sand 1/16 - 2mm Sand Sandstone

    Silt 1/256 - 1/16 mm

    Silt Siltstone

    Clay

  • Sedimentary Texture

    1. Grain Size

    = energi transportasi,

    see Wentworth scale

    2. Sortasi

    = keseragaman ukuran butir

    v.w. sorted-w.sorted-m.sorted-p.sorted

  • Coarser-grained,

    Very poorly sorted

    Finer-grained,

    moderately sorted

    Lower

    K

    Higher

    K

  • Yellow = grains The two areas are equal

    Purple = pores

    Thicker bedded, less grain contact

    Higher permeability

    Thinner bedded, more grain contact,

    Lower permebility

  • 3. Bentuk Butir

    Tingkat Pembolaan (sphericity)

    high sphericity low sphericity

    Tingkat Kebundaran (roundness)

    v.angular well rounded

    Surface Texture

    (permukaan halus permukaan kasar)

  • 4. Kemas (Fabric)

    = Orientasi dan hubungan antar butir (packing)

    Orientasi Flow Direction

    Packing Grain supported Matrix supported