FIELD TRIP YOGYAKARTA, 20 JULY 2017 (CCOP, GEOLOGICAL AGENCY)

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I$neraryFieldTripofCCOPinYogyakarta,20July2017# Time Item Person/Organiza3on

1. 07.30–09.00 StartfromYogyakartatoStopSite1 AllPar$cipants

2. 09.00–10.00 Discussinstopsite1 AllPar$cipants

3. 10.00–10.30 Gotostopsite2 AllPar$cipants

4. 10.30–11.15 Discussinstopsite2 AllPar$cipants

5. 11.15–11.45 GotoRawaJombor AllPar$cipants

6. 11.42–14.00 LunchinRawaJombor AllPar$cipants

7. 14.00–14.45 GotoPrambananTemple AllPar$cipants

8. 14.45–16.45 PrambananTemple AllPar$cipants

9. 16.45–17.30 GotoYogyakarta AllPar$cipants

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FieldTripMapofCCOPYogyakarta2017TrackofFieldTripCCOPYogyakarta,2017;

1.  StopSite1(KeboButakForma$on)

2.  StopSite2(GampingWungkalForma$on)

3.  StopSite3(RawaJombor)

4.  StopSite4(PrambananTemple)

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Loca$onandStra$graphicofBayat

(Suronodkk.,1992) (Husein,2014)

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StopSite1/KebobutakForma$on

Claystone-Sandstone

VolcanicRock

KebobutakForma$ondeposited

on Late Oligocene – Early

Miocene, that cons ist of

sandstone, si ltstone, grey

claystone, and black claystone

at the lower part. At the upper

part consist of volcanic rock,

Thickness of this forma$on

morethan600m.

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Claystone-Sandstone

VulcanicRock

StopSite1/KebobutakForma$on

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StopSite2/GampingWungkalForma$onWungkal Gamping Forma$on

deposited on Middle Eocene –

Late Eocene, that consist of

l imestone with abundant

Nummul ites foss i l as the

characteris$c of Eocene. The

thickness of this forma$on

about 120 m and deposited in

shallow marine with rich fossil,

then s l ide down and re-

deposited in the deep sea,

therefore this forma$on is

‘exo$cfaunalassemblage’.

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StopSite2/GampingWungkalForma$on

Nummulites

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StopSite3/RawaJombor

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StopSite4/PrambananTemple

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REPUBLIK INDONESIA