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Sedimentary microfacies of the H8 member in the Su14 3D seismic test area.pdf
MiningScienceandTechnology(China)21(2011)233-237
。警一。薯镪 毫毫。董誊≯曩 毫。零 m s B 贰 毓s 讯 钒 _§、 _ l
--| 朋鼬 一 a刃 fJ冽 _
囊一|薯 誉 je叠薯誊 曩誊蚤 霪攀 |毫疆 ≯ 嚣《尊蕊嚣|
| j蠢 蘩一霪 ≯ l_ lll_
EL咖 ER ; 誊s ,Dw,,a,沁m8pag彰iw e,卯 ,茸,io, 归 伽sfc ll ■
A R T lC L E IN F O A B S T R A C T
Articlehistory: ThedistributionofsedimentarymicrofaciesintheeighthmemberoftheShiheziformation (theH8
Received13August2010 member)intheSu143Dseismictestareawasinvestigated.ASuppo~VectorMachine(SVM)modelwas
Receivedinrevisedform
introducedforthefirsttimeasawayofpredictingsandstonethicknessinthestudyarea.Themodelwas
30September2010
constructedbyanalysisandoptimizationofmeasuredseismicattributes.Thedis仃ibutionofthesedi-
Accepted28October2010
mentan,microfaciesin the sutdyareawasdeterminedfrom predicted sandstonethicknessandan
analysisofsedimentary characteristicsofthearea.Th eresultsindicatethatsandstonethickness
Keywords:
predictionsin thesutdyareausingan SVM methodaregood.Thedistribution ofthesedimentary
SVM
microfaciesinthestudyareahasbeendepictedatafinescale.
Seismicattribute
Sandstonethickness Copyright@ 2011.ChinaUniversityofMining&Technology.AIlrightsreserved.
Sedimentarymicrofacies
3D seismictestarea
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