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  • Tectonic post-collision processes in Timor - earthjay
    This paper discusses the key geological processes associated with the Timor tectonic collision Timor Island has mountains up to 3 km high, is over 475 km long and has a width of 75–100 km (150 km wide with its submarine southern slope) Without including the volcanic islands, East and West Timor are together larger than the 280 100 km Swiss Alps The Banda Arcs are 2300 km long, a length
  • (PDF) Geological Development of the Timor Orogen - ResearchGate
    Vertical loading and the southerly motion of the orogenic wedge are the main driving forces responsible for its building, illustrating a thin-skinned tectonic framework
  • Integrated geological and geophysical interpretation of the complex . . .
    The complex geology of Timor orogen is here addressed with an integrated Geological and Geophysical interpretation At the surface, the aeroradiometric maps are correlated with the geological data to address the complex geology map At the subsurface, the aeromagnetic and aerogravity maps are spatially and vertically interpreted and integrated with the geological data to address the geological
  • Geological development of the Timor Orogen - Geological Society, London . . .
    Seismic interpretation of the dataset demonstrated structural and tectonic features not previously described, including regional geological features on the Australian continental crust and two regional NE–SW sinistral strike-slip faults, and a prominent Middle Permian palaeogeographical high (Timor Plateau)
  • Strike-slip tectonics in arc-continent collision; the Eastern Timor example
    This mapping was part of a cooperation project between the Secretaria de Estado dos Recursos Naturais (SERN) of Eastern Timor and the Évora University (Portugal) and will be part of the new Manatuto 1 50 000 geological map
  • On-going orogeny in the outer-arc of the Timor . . . - ScienceDirect
    The Timor–Tanimbar islands of eastern Indonesia form a non-volcanic arc in front of a 7 km deep fore-arc basin that separates it from a volcanic inner arc The Timor–Tanimbar Islands expose one of the youngest high P T metamorphic belts in the world, providing us with an excellent opportunity to study the inception of orogenic processes, undisturbed by later tectonic events
  • The geology of Timor-Leste: a review - Zenodo
    The island of Timor is part of the Outer Non-Volcanic Banda Arc that is formed on the collision zone between the Volcanic Banda Arc and Australian Continental Crust (Carter et al , 1976; Barber et al , 1977; Audley-Charles, 2004) Banda Arc is a horse-shoe-shaped island arc, which forms 180-degree curve situated in Eastern Indonesia (Figure 1 1), between three major tectonic plates - India
  • Geological development of the Timor Orogen - GeoScienceWorld
    The Timor Orogen comprises the island of Timor, a narrow offshore area to the north and a wider offshore fold-and-thrust belt to the south This orogen formed by jamming and subsequent collision of the Banda Sea subduction system by the Australian Plate
  • Triassic Massive Limestones Forming High Peaks and Mountain Ranges in . . .
    Also shown are dismembered blocks of OTA that collided with and were emplaced onto the Timor margin of the Australian continent during orogenesis that commenced during the Late Miocene Lower right: present-day tectonic setting of Timor
  • Giliam Hamson - The Tectonic Evolution of East Timor and The Band
    This document provides an overview of the geology and tectonic evolution of East Timor and the Banda Arc region It discusses the complex geology of East Timor, which includes rocks derived from the Australian continental margin as well as the Banda forearc





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