Sorong Fault Zone is located at northern of the Papua Island. It is moving from the body bird of Papua Island toward south-southeast of Molluca Island, spreading to east part of Celebes Island, and overstepping east part of Yapen Island which occupied the Bird’s Neck of Papua. The fault became a border between Caroline oceanic plate (part of pacific oceanic plate) and Australian continental plate. Instead, The Sorong Fault Zone controlled forming of Salawati Basin in west of Yapen Island. The Sorong Fault, Lengguru Fold thrust belt, Tarera-Aiduna Fault, and Seram Thrust are structural features which associated with the collision between the Australian continental plate and the Pacific oceanic plate at Oligo-Miocene as regional uplift.This p...
Middle Miocene onwards, the Banda Sea started to be devolved due to retreat and roll-back of the nor...
DOI: 10.17014/ijog.5.2.137-160A detailed active fault study in Tarutung-Sarulla-Sipirok-Padangsidemp...
Located approximately a hundred kilometres north of Java Subduction Zone, Java Island has a complica...
Indonesia, are two sedimentary basins located either side of the main fault strands in the Sorong fa...
This thesis aims to establish how the late Cenozoic oblique convergence of the Pacific- Caroline and...
DOI:10.17014/ijog.3.1.1-16Most of the Cenozoic tectonic evolution in New Guinea is a result of obliq...
Papua and Papua New Guinea are had geology condition are very complex involving interaction between ...
<div><p>The Owen Stanley Fault Zone (OSFZ) is the low-angle thrust boundary between the Australian a...
The Philippine Sea Plate is the one major plate whose Tertiary motion is poorly constrained and whos...
Gedangan area is situated in HargoMulyo, Gedangsari District, Gunung Kidul Regency, Special Region o...
Study area is located in South Banda Basin near the triple junction between Eurasian, Pacific and In...
The boundary between the Philippine Sea and Australian plates is the left-lateral Sorong Fault syste...
Gravity surveys along coastlines of islands in the region Banggai-Sula, Eastern Sulawesi, Halmahera,...
The Philippine Sea Plate is the one major plate whose Tertiary motion is poorly constrained and whos...
Since ~ 25 Ma ago the plate margin between the Australian plate and the Philippine Sea and Pacific-C...
Middle Miocene onwards, the Banda Sea started to be devolved due to retreat and roll-back of the nor...
DOI: 10.17014/ijog.5.2.137-160A detailed active fault study in Tarutung-Sarulla-Sipirok-Padangsidemp...
Located approximately a hundred kilometres north of Java Subduction Zone, Java Island has a complica...
Indonesia, are two sedimentary basins located either side of the main fault strands in the Sorong fa...
This thesis aims to establish how the late Cenozoic oblique convergence of the Pacific- Caroline and...
DOI:10.17014/ijog.3.1.1-16Most of the Cenozoic tectonic evolution in New Guinea is a result of obliq...
Papua and Papua New Guinea are had geology condition are very complex involving interaction between ...
<div><p>The Owen Stanley Fault Zone (OSFZ) is the low-angle thrust boundary between the Australian a...
The Philippine Sea Plate is the one major plate whose Tertiary motion is poorly constrained and whos...
Gedangan area is situated in HargoMulyo, Gedangsari District, Gunung Kidul Regency, Special Region o...
Study area is located in South Banda Basin near the triple junction between Eurasian, Pacific and In...
The boundary between the Philippine Sea and Australian plates is the left-lateral Sorong Fault syste...
Gravity surveys along coastlines of islands in the region Banggai-Sula, Eastern Sulawesi, Halmahera,...
The Philippine Sea Plate is the one major plate whose Tertiary motion is poorly constrained and whos...
Since ~ 25 Ma ago the plate margin between the Australian plate and the Philippine Sea and Pacific-C...
Middle Miocene onwards, the Banda Sea started to be devolved due to retreat and roll-back of the nor...
DOI: 10.17014/ijog.5.2.137-160A detailed active fault study in Tarutung-Sarulla-Sipirok-Padangsidemp...
Located approximately a hundred kilometres north of Java Subduction Zone, Java Island has a complica...