%0 Conference Paper
%A Bernadeta Subandini Astuti, .
%B The 2nd Join Conference of Utsunomiya University and Universitas Padjadjaran, Nov.24,2017
%C Universitas Padjadjaran Bandung
%D 2017
%F ITNYREPOID:3063
%K Rambatan Formation, North Serayu basin, Tectonic, slump
%P 233-237
%T PEER REVIEW : MICRO TECTONIC AT NORTH SERAYU BASIN, CENTRAL JAVA:  CASE STUDY AT TYPE LOCALITY OF RAMBATAN FORMATION
%U https://repository.itny.ac.id/id/eprint/3063/
%X Type location of Rambatan Formation at Pamulihan, Larangan, Brebes, Jawa Tengah,  Rambatan Formation occupies in North Serayu Basin. Regional character of Rambatan  Formation is deep marine flysch or turbidity current as lower fan. Tectonic active  controlled lithology of Rambatan Formation that is quick subsidence at Early Miocene to  Late Miocene. Tectonic during Middle Miocene to Pliocene caused the change of sea level  three times. Change of sea level, tectonic and supply sediment is related to dynamic  sedimentation in basin. The presence of turbidite in general is always associated with  hydrocarbon potential. Potential of hydrocarbon in research area are supported by oil  seepage. Analysis of micro tectonic will be part of the sedimentation dynamic that is  related play hydrocarbon. Tectonic active in type location of Rambatan Formation take  place at early Late Miocene (N15 to N16). That bordered between relative deeper marine  and shallow marine. Shallow marine begins with the presence of slump at N17. Indication  of tectonic are unconformity, change of environmental (deep water and shallow water), and  fault association. The dynamics of sedimentation toward tectonic N15 to N16 will be  related to the accommodation space. Accommodation space in research area is decrease. It  is marked by the environmental change from deeper to shallow marine that is followed by  decrease of sea level and increase sedimentation from south