bentukan log

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  • 7/23/2019 bentukan log

    1/4

    PROGRADATIONAL

    (Regressive, Seaward -

    Stepping)

    RETROGRADATIONAL

    (Backstepping, Transgressive,

    Landward-Stepping)

    AGGRADATIONAL

    Thicker, less shaly upward

    Sediment source moving closer (regression)

    Typical of HIGHSTAND systems tract

    Similar thickness, shaliness

    Sediment source maintained nearby

    Typical of LOWSTAND systems tract

    Upward thinning, shalier

    Sediment source moving away (transgression)

    Typical of TRANSGRESSIVE systems tract

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    Changes in these patterns can be used for sequence stratigraphic interpretation and

    correlation

    Flooding Surface/

    Sequence Boundar

    !a"i#u# Flooding

    Surface

    $ncise

    d

    %alleSequenc

    e

    Boundar

    &ig'stand is

    #issing,

    proal erodedawa

    Lowstand is #issing,

    proal an interfluve

    TST

    LST

    TST

    TST

    TST

    LST/TST

    LST

    &ST

    Idealized parasequence stacking patterns of a complete marginal marine depositional

    sequence

    !a"i#u# Flooding

    Surface

    Transgressive Surface

    &ig'stand*

    +rogradational

    Transgressive*

    Retrogradational

    Lowstand*

    ggradational

    &ig'stand*

    +rogradational

    Sequence Boundar

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    2

    0

    12

    0

    -

    2150

    m

    -

    2175

    m

    -2200

    m

    -

    2225

    m

    -

    2250

    m

    G

    R

    Aggradational succession

    possible composite incised valley fill

    Progradational to Retrogradational -

    shorefacedeltaic deposits

    Aggradational to retrogradational succession

    valley fill! Channel fill overlain by delta lobes!

    "equence#oundary!

    $a%imum

    &looding "urface

    Cored

    interval

    *

    An example from Southeast Asia

    $a%imum

    &looding "urface!

    $a%imum

    &looding "urface

    "equence#oundary!

    Lowstand-TransgressiveSystems Tract?

    Lowstand-

    TransgressiveSystems Tract?

    Highstand

    Systems Tract?

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    -

    2200

    m

    -

    2225

    m

    -2350

    m

    -

    2375

    m

    -

    2250

    m

    -

    2275

    m

    -

    2300

    m

    -

    2325

    m

    -

    2400

    m

    2

    0

    12

    0

    2

    0

    12

    0

    G

    R

    G

    R

    !a"i#u# Flooding

    Surface

    !a"i#u# Flooding

    Surface

    !a"i#u# Flooding

    Surface

    Cored

    interval!a"i#u# Flooding

    Surface

    !a"i#u# Flooding

    Surface

    $a%imum

    &looding

    "urface!

    Transgressive

    Systems Tract

    Transgressive

    Systems Tract

    Highstand

    Systems TractHighstand

    Systems Tract

    HighstandSystems Tract