Basic Sikuenstratigrafi
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Transcript of Basic Sikuenstratigrafi
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SIKUENSTRATIGRAFI
Penggolongan lapisan batuan secarabersistem menjadi satuan bernamaberdasarkan satuan genesa ang dibatasi!
di bagian ba"a# dan atasna! ole# bidangketidakselarasan atau keselarasanpadananna$
Satuan sikuenstratigra% iala# suatu tubu#lapisan batuan ang terbentuk dalamsatuan "aktu pada satu daur peruba#anmula&laut relati'$
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(atas Satuan
• (idang ketidakselarasan) bidangerosi! pada umumna terjadi di atasmuka laut *sub&aerial+! ditandai ole#
rumpang "aktu geologi$
• (idang keselarasan padanan) bidangkelanjutan dari bidang
ketidakselarasan ke ara# susunanlapisan batuan ang selaras$
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Tingkat&tingkat Satuan
• ,ari besar sampai kecil -.egasikuen / Supersikuen / Sikuen
• Sikuen adala# satuan dasar dalampembagian satuan sikuenstratigra%$
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Uncon'ormities
Stratigrap#ic sur'aces across "#ic#t#ere is e0idence 'or a signi%canttime gap$
- Angular uncon'ormities
- ,iscon'ormities
- Paracon'ormities
- noncon'ormities
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Inclusion principle) T#e 'ragment ina clastic rock must be made up o' arock t#at is older t#an t#e strata in"#ic# t#e are 'ound$
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1#at is 'acies2
In stratigrap#! a facies is a bod o'p#sical c#aracteristics t#at allo" toattribute a sediment to a speci%c
depositional en0ironment 'ordistinction 'rom adjacent sedimentdeposited in a di3erent depositional
en0ironment$Sedimentar 'acies re4ectdepositional environment$
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5the verticalsuccession offacies reectslateral
migration inenvironment because "#en adepositional
en0ironmentmigrateslaterall!sediments ofonedepositional
Walther’s Law of FaciesSuccession:
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A transgression occurs "#en t#e rate o'sea le0el rise land"ard e6ceeds t#e rate o'
sediment input! and causes an increase inaccomodation$
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A regression occurs "#en sedimentationrates outpace t#e rates o' base & le0el rise at
t#e s#oreline! or "#en base&le0el 'alls$
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Cyclicity)
.uc# o' t#e sedimentar recordsdispla e0idence 'or repetiti0etransgressi0e7regressi0e episodes$
Transgression and regressions causedb t#e interpla o')
- Gloal sea level change
- !ectonic susidence"uplift- Changes in sediment supply
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8onse9uences o' sea le0elc#ange
• (ased on Embr *:;;:+
• 8#anges in 5depositional trend<
•
T"o main possibilities)=$ 8#ange 'rom deposition to erosion
:$ 8#ange 'rom s#allo"ing up"ard
trend to deepening up"ard trend
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8onse9uences o' Sea >e0el8#ange
• (ase le0el 'all)
- Sediment accumulation ceasealong basin margin! subaerialerosion sur'ace e6pandsbasin"ard$
- Sea / 4oor erosion on inner s#el' in
ad0ance o' prograding s#oreline$
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8onse9uences o' Sea >e0el8#ange
• (ase le0el rise)
- Accumulation o' non&marine strataspreads in a land"ard direction abo0e
a subaerial erosion sur'ace$
- 8#ange 'rom regressi0e trend to atransgressi0e trend in marine deposits$
- ,eposition ceases at s#oreline anderosion at s#oreline starts$
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:?
Transgressive sequence set = retrogradational sequence set
Highstand sequence set = progradational sequence set
Lowstand sequence set