Ransiki Fault News Today : Breaking News, Live Updates & Top Stories | Vimarsana

Stay updated with breaking news from Ransiki fault. Get real-time updates on events, politics, business, and more. Visit us for reliable news and exclusive interviews.

Top News In Ransiki Fault Today - Breaking & Trending Today

"Ransiki earthquakes, northeastern Bird's Head Peninsula, northwestern " by Sukahar Eka Adi Saputra, Christopher L. Fergusson et al.

The plate boundary between the Pacific-Caroline and Australian plates in northwestern New Guinea is associated with a geographic concentration of earthquakes developed in the Ransiki region of the northeastern Bird's Head Peninsula (West Papua, northwestern New Guinea) at the intersection of the Ransiki and Yapen faults. We examine these earthquakes based on regional geomorphological and lithostratigraphical frameworks, field observations of surface ruptures and liquefaction phenomena, and focal mechanisms of historical earthquakes. The Ransiki earthquakes are a set of 29 earthquakes from the Global Centroid Moment Tensor catalogue in the period 1977–2019 (magnitudes of Mw4.9 to Mw7.5). In the east, focal mechanisms show sinistral movement along the east-west trending Yapen Fault including the Mw6.7 earthquake on 21 April 2012. The largest earthquake was on 10 October 2002 (Mw7.5) and along with other earthquakes mainly in the southwest were associated with dextral movement indi ....

Irian Jaya Barat , Indonesia General , West Papua , New Guinea , Head Peninsula , Global Centroid Moment Tensor , Yapen Fault , Ransiki Fault , Wainoei Fault , Deformation Partitioning , Eastern Indonesia , Ault Intersection , Local Mechanisms ,

"Neogene uplift and deformation in the northeastern Bird's Head Peninsu" by Sukahar Eka Adi Saputra, Christopher L. Fergusson et al.

Since ~ 25 Ma ago the plate margin between the Australian plate and the Philippine Sea and Pacific-Caroline plates in northwestern New Guinea has been undergoing oblique convergence and resulted in various uplifts and compressional deformation in the Bird’s Head Peninsula. These reflect partitioning into north-northeast compression and east-west sinistral strike-slip faulting analogous to that in the Sumatran active margin. We present new data on the provenance of the upper Miocene to lower Pliocene succession in the northeastern Bird’s Head Peninsula and its structure that has enabled a new tectonic synthesis. Initiation of oblique convergence resulted in development of the sinistral strike-slip Sorong Fault and docking of the Oligocene Arfak Volcanics from the southern Philippine Sea Plate. At ~ 15–12 Ma the compressional component initiated 40 km of dextral offset of the Sorong Fault along the northwest-trending Ransiki Fault. Subsequently, sinistral movement along the Sorong ....

Philippine Sea , Oceans General , New Guinea , Head Peninsula , Sorong Fault , Oligocene Arfak Volcanics , Ransiki Fault , Birds Head Peninsula , Etritalu Pb Zircon Ages , Oblique Convergence , Strike Slip Faults ,

"Cenozoic deformation and tectonics of eastern Bird's Head Peninsula, W" by Sukahar Eka Adi Saputra

This thesis aims to establish how the late Cenozoic oblique convergence of the Pacific- Caroline and Australian plates has affected the tectonic history of the eastern Bird’s Head Peninsula in northwestern New Guinea. Emphasis is placed on insights provided by >5 magnitude earthquakes since 1976 and the structural geology of Miocene-Pleistocene sediments in the Manokwari area and Permian to Paleogene units of the northern Lengguru Fold Belt around Mawi Bay. The Bird's Head Peninsula is moving west- southwest relative to the Australian Plate based on GPS data, but slower than the west- southwest movement of the Pacific-Caroline Plate. This accounts for plate convergence between the Pacific-Caroline Plate and the Bird's Head Peninsula consistent with earthquakes caused by gently south dipping thrusts in an arc along the northern Bird’s Head coastline and indicating subduction along the Manokwari Trough. Southwards subduction along the New Guinea Trench to the northeast o ....

Head Peninsula , Lengguru Fold Belt , Australian Plate , Pacific Caroline Plate , New Guinea Trench , Yapen Island , Yapen Fault , Cendrawasih Bay , Sorong Fault , Kemum High , Tarera Aiduna Fault , Pleistocene Manokwari Limestone , Ransiki Fault , Permian Mawi Complex , Upper Triassic , Lower Jurassic Tipuma , Late Permian , Early Triassic , East Gondwanan Andean , Mawi Complex , Pliocene Lengguru Fold , Central Bird , Head Monocline , Oblique Convergence , Birds Head ,