Structure of regional Balinese geology was begun with the existence of the activity in the ocean for time of Miosen Under that produced the rock of pillow lava and breksi that inserten by the limestone.
On the south the sedimentation happened by the limestone that afterwards formed the South Formation. In the route that shared a border with his north bank the softer sediment sedimentation happened. At the end Pliosen time, all the area of the sedimentation emerged above sea level. Along with the appointment, the shift that caused various parts to be moved aside happened one against that was other. Generally this fault sank by the organic rock material or younger sediment.
For Pliosen time, in the next ocean north sediment happened took the form of the material that came from sediment that afterwards produced the Asah Formation. In west sea some of the rocks emerged onto sea level. Now this increasingly to west the sedimentation of the carbonate rock was more dominant. All the route was at the end of Pliosen lifted and moved aside.
The volcano activity more often happened in the mainland, that produced the volcano from the west to the east. Together with the occurrence of two calderas, that is at first the caldera of Buyan - Bratan and afterwards the Shelf caldera, Balinese Island was still experiencing the movement that caused the appointment on the north. As a result, the Palasari Formation is promoted to sea level and the Balinese Island generally had the North-south not symmetrical profile. The southern part more the gradient from the north.
Regional stratigraphy was based on the Map of Balinese Geology, Balinese geology be classed as still was young. The eldest rock the possibility be aged Middle Miosen.
On the south the sedimentation happened by the limestone that afterwards formed the South Formation. In the route that shared a border with his north bank the softer sediment sedimentation happened. At the end Pliosen time, all the area of the sedimentation emerged above sea level. Along with the appointment, the shift that caused various parts to be moved aside happened one against that was other. Generally this fault sank by the organic rock material or younger sediment.
For Pliosen time, in the next ocean north sediment happened took the form of the material that came from sediment that afterwards produced the Asah Formation. In west sea some of the rocks emerged onto sea level. Now this increasingly to west the sedimentation of the carbonate rock was more dominant. All the route was at the end of Pliosen lifted and moved aside.
The volcano activity more often happened in the mainland, that produced the volcano from the west to the east. Together with the occurrence of two calderas, that is at first the caldera of Buyan - Bratan and afterwards the Shelf caldera, Balinese Island was still experiencing the movement that caused the appointment on the north. As a result, the Palasari Formation is promoted to sea level and the Balinese Island generally had the North-south not symmetrical profile. The southern part more the gradient from the north.
Regional stratigraphy was based on the Map of Balinese Geology, Balinese geology be classed as still was young. The eldest rock the possibility be aged Middle Miosen.
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