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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)
5
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$on
morethan600m.
7
StopSite2/GampingWungkalForma$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’.