Analisis sekuen stratigrafi dan fasies batugamping, formasi lower nguimbing, cekungan Jawa Timur Utara
D aerah penelitian terletak pada lapangan FA, Cekungan Jawa Timur Utara.Total sumur yang dianalisis berjumlah tiga sumur, yaitu sumur FA-1, FA-2 dan FA-3. Tujuan dari penelitian ini adalah untuk menganalisis fasies dan sikuen stratigrafibatuan karbonat secara vertikal, maupun horizontal. Metode yang digunakan adalahanalisis litofasies, analisis reef system dan analisis sikuen stratigrafi denganmenggunakan data core (berupa foto sayatan tipis petrografi), data log dan dataseismik. Berdasarkan analisis sekuen stratigafi pada daerah penelitian maka terdapatdua sekuen yang di batasi oleh 3 SB dan 2 MFS dan Berdasarkan litofasies padadaerah peneltian maka dapat dibagi mejadi enam fasies yaitu Coralline Boundstone,Red Algae Packestone, Red Algae Grainstone, Bioclast Wackestone To Packestone,Large Foram Skeletal Packestone dan , Bioclast - Intraclast Wackestone ToPackestone. Selain itu pada sumur FA-1, 2 dan 3 terdapat dua reef system yaitu, reefcore, dan fore reef dan dua fasies sesmik yaitu platform slope dan platform interior
T he research area is located in FA field, North East Java Basin. FA field containsthree well such as FA-1, FA-2 and FA-3. The purpose of this research is to analyzefacies and sequence stratigraphic of carbonate rock vertically, or horizontally.Several methods are analysis lithofacies, analysis, analysis reef system and analysissequence stratigraphy based on core (photo of thin section petrography), log andseismic. analysis result based on sequence stratigaphy analysis on the research showsthere are two sequence which is restricted by 3 SB and 2 MFS and the analysis resultbased on lithofaces analysis shows there are six types of facies which are CorallineBoundstone, Red Algae Packestone, Red Algae Grainstone, Bioclast Wackestone ToPackestone, Large Foram Skeletal Packestone and Bioclast - Intraclast WackestoneTo Packestone. There are two types of reef system such as reef core, and fore reefand two facies seismic such as platform slope and platform interior.