منابع مشابه
Rift migration explains continental margin asymmetry and crustal hyper-extension
When continents break apart, continental crust and lithosphere are thinned until break-up is achieved and an oceanic basin is formed. The most remarkable and least understood structures associated with this process are up to 200 km wide areas of hyper-extended continental crust, which are partitioned between conjugate margins with pronounced asymmetry. Here we show, using high-resolution thermo...
متن کاملContinental rift
The azure-winged magpie (Cyanopica cyanus), has long presented a puzzle for biologists. The naturalist Alfred Wallace was one of the first to consider it. The puzzle lies in its extraordinary distribution. It exists in two distinct locations: Iberia and eastern Asia, 9,000 kilometres apart. Two alternative theories have been put forward to explain this curious distribution. The first proposes t...
متن کاملCrustal structure and rift flank uplift of the Adare Trough, Antarctica
[1] The Adare Trough, located 100 km northeast of Cape Adare, Antarctica, represents the extinct third arm of a Tertiary spreading ridge between East and West Antarctica. It is characterized by pronounced asymmetric rift flanks elevated up to over 2 km above the trough’s basement, accompanied by a large positive mantle Bouguer anomaly. On the basis of recently acquired seismic reflection and sh...
متن کاملContinental drift and plateau uplift control origination and evolution of Asian and Australian monsoons
Evolutions of Asian and Australian monsoons have important significance for understanding the past global change but are still a controversial subject. Here, we explore systematically the effects of plate movement and plateau uplift on the formation and evolution of the Asian and Australian monsoons by numerical simulations based on land-sea distributions and topographic conditions for five typ...
متن کاملSmall-scale convection induced by passive rifting: the cause for uplift of rift shoulders
Areas adjacent to rifts, or rift shoulders, are often observed to be uplifted as much as a kilometer or more. In some of these regions geologic data indicate a passive origin for the rifting itself (i.e. there was no anomalous heating of the regions before rifting). Purely conductive heat transport between the rift, where the lithosphere has been thinned, and the rift flanks cannot account for ...
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ژورنال
عنوان ژورنال: Tectonics
سال: 2003
ISSN: 0278-7407
DOI: 10.1029/2002tc001459