Sedimentasi pada umur Permian hingg

Sedimentasi pada umur Permian hingga Jurassic di dominasi oleh endapan siliklastik. Litologi Permian didominasi shale, sandstone dan coal yang dikenal sebagai formasi Aiduna, Aifat, dan Ainim. Pada umur Paleosen, daerah Tangguh didominasi oleh endapan shelf hingga laut dalam. Endapan submarinefan yang berupa batupasir merupakan reservoir sekunder di daerah Tangguh. Tumbukan pada umur Oligo-Miosen telah mengangkat daerah ini dan menambah input sedimentasi. Formasi Klasafet dan Steenkol diendapkan pada periode setelah tumbukan

Results (English) 1:

Sedimentation in the Permian to Jurassic age dominated by sediment siliklastik. Lithology dominated Permian shale, sandstone and coal formations known as Aiduna, Aifat, and Ainim. In the Paleocene age, the area is dominated by sediment Tough shelf to the deep sea. Submarinefan precipitate in the form of a secondary reservoir sandstones are in the area Tangguh. The collision of the Oligo-Miocene age has elevated this area and add input sedimentation. Klasafet and Steenkol formations deposited in the period after the collision

Results (English) 2:

Sedimentation at the Permian to Jurassic age in domination by siliklastic deposition. The Permian Litology is dominated by shale, sandstone and coal, known as Aiduna, Aifat, and Ainim formations. At the Paleocene age, the Tangguh area is dominated by shelf-to-deep seas. Deposits of Submarinefan in the form of a sandstones are secondary reservoirs in the Tangguh area. Collids at the age of Oligo-Miocene have raised this area and added sedimentation inputs. Klasafet and Steenkol formations were deposited in the period after the collision

Results (English) 3:

Sedimentasi pada umur Permian hingga Jurassic di dominasi oleh endapan siliclastik. Litologists Permian didominasi shale, sandstone dan coal yang dikenal sebagai formasi Aiduna, Aifat, dan Ainim. It falls on the shoulders of the Paleos, so that Tangguh didominasi oleh endapan shelf hingga laut dalam. Endapan submarinefan yang drunk batupasir merupakan reservoir seconds di daerah tangguh. Tumbukan falls dead Oligo-Miosen bodies intermingkat daerah ini dan menambah input sedimentasi. Formasis Classical day Stone diendapkan decreases period of set tumours