basin vs plate tektonik(1a)

7/17/2019 Basin vs Plate Tektonik(1a)

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eddy purnomo 4 unpad bdg

PRINSIP DASAR CEKUNGAN SEDIMENPRINSIP DASAR CEKUNGAN SEDIMEN

eddy purnomo / 620438

jatinangor september 2006


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MATERI KUIA!

PENDAHULUAN

PRINSIP2 DASAR E!UN"AN SEDI#EN

Ce"#ngan se$imen %s P&ate te'toni'Me"ani"a &it(os)er

#E!ANIS#E PE#$EN%U!AN E!UN"AN SEDI#ENit(osperi' stret'(ing*&e+#re

Stri"e s&ip $e)ormation

%HE SEDI#EN%AR& $ASIN 'ILL*a"tor pengontro&Depositiona& st,&e

E()LUSI E!UN"AN SEDI#ENS#bsi$en'e (istor,T(erma& (istor,

APLI!ASI DALA# INDUS%RI E * P #I"AS


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CEKUNGAN SEDIMEN -S PATE TECT.NIC

.'eani' Cr#st %s Continenta& Cr#st

Intra'ratoni' %s P&ate Margin

Po&a Te"toni"


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CEKUNGAN SEDIMEN

No Subsidence, No Sedimentary Basin

No Sedimentary Basin, No HydrocarbonNo Hydrocarbon, No Modern Civilization


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SU/SIDENCE

Subsidence ~ Plate motion (Interaksi

antar em!en"#ateral Movement ~ $ertical Movement

%e&ormasi se!an'an" Plate Boundaries


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INTERAKSI ANTAR EMPENG

Salin" men'au

Salin" mendekatSalin" ber!a!asan


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CURRENT MAJOR TECTONIC PLATES


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M)*+NISM) P)MB)N-*+N C)*-N.+N

B)/%+S+/*+N *0N%ISI IH0S1)/)


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P&ate Te'toni' 'on'ept#a& mo$e& o) basin e%otion

Ri)ting

Passi%e Margin

A'ti%e Margin

Is&an$ ar'

Co&&ision

Continent


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PLATE TECTONIC CONCEPT

AND PRINCIPLE ARE ABLE TO :

EXPLAIN EXPLAIN

BASIN

DEFORMATION

DURING-AFTER

SEDIMENT.

STRUCTURATION

STRUCTURAL

PATTERN

OBSERVED/PREDICTED

BASIN

FORMATION

BASIN TYPE

STRATIGRAPHIC

SEQUENCES

OBSERVED/PREDICTED

CHART SHOWING RELATION BETWEEN BASIN FORMATIONDEFORMATION AND PLATE TECTONIC (TEKTONIK)

EXPLORATION

STRATEGY

PETROLEUMSYSTEM

HYDROCARBONPOTENTIAL

RESULTED IN BASIN CHARACTERISTICS

PREDICT


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MODERN

BASIN

GROUP OF BASINS

BASED ON PLATE TECTONIC SETTING

ANCIENT

BASIN

STILL OCCUPY

THE SAME PLATE

TECTONIC POSITION

AS THEY DID

WHEN FORMED

BASINS FLANKING

THE ATLANTIC

OCEAN

THE PLATE

TECTONIC SETTING HAS

UNDERGONE SEVERAL

CHANGES

SINCE THEY

FORMED

BASINS IN THE

NORTH AMERICAN

CORDILLERA

CLASSIFICATION AND

NOMENCLATURE APPLIED IS BASED ON THEIR

PLATE TECTONIC SETTING AND DEVELOPMENT


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C.ISI.N

PASSI-E

C.NTINENTA

MARGIN

ISAND ARC

ACTII-E

C.NINENTAMARGIN


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PLATE TECTONIC SETTING

.'eani' 'r#st MID ATANTIC

RIDGEANDES

EAST PACI*IC

RISE2a!an +rc

E#rasian P&ate

!ima&a,a

Trans)orm )a#&t

Is&an$ Ar'

ANDES

E#rasian P&ate

C.N-ERGING1 DI-ERGING1DI-ERGING1

C.N-ERGING1DI-ERGING1

C.N-ERGING1

C.N-ERGING1

PLATE MARGIN

PLATE MARGIN

PLATE INTERIOR

CLASSIFICATION AND

NOMENCLATURE APPLIED IS BASED ON THEIR

PLATE TECTONIC SETTING AND DEVELOPMENT


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KINGSTON et.al


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Tectonic Ee!ent" o# In$one"i%Tectonic Ee!ent" o# In$one"i%


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TERIMA KASI!TERIMA KASI!

'atinan"or, oktober 3445


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basin vs plate tektonik(1a)

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