The origin of adakite-like magmas in the modern continental ollision zone: evidence from pliocene dacitic volcanism of the Akhalkalaki lava plateau (Javakheti highland, Lesser Kaucasus) [PDF]
V. А. Lebedev +3 more
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Early Stages Arc Volcanism in the Eastern Himalayan Synstaxis, Yarlung Zongbo Suture Zone, Tibet, China: New Zircon Age, Hf Isotopic, Geochemical Constrains and Implication for the Tectonic Evolution History of Neo‐Tethys [PDF]
Yuan Li +5 more
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Relations between the northern and southern margins of the Tethys ocean during the Cretaceous period
A set of 11 abstracts and short papers (extended abstracts) of presentations given at a meeting organized by the "Groupe Français du Crétacé (GFC)", held on November 27-28, 2007 at the "École des Mines" in Paris ...
Bulot Luc G. +2 more
doaj
The Holocene volcanism of Gran Canaria (Canary Islands, Spain) [PDF]
Alejandro Rodríguez-González +5 more
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Ages on weathered Plio-Pleistocene tephra sequences, western North Island, New Zealand [PDF]
Using the zircon fission-track method, we have obtained five ages on members of two strongly-weathered silicic, Pliocene-Pleistocene tephra sequences, the Kauroa and Hamilton Ash formations, in western North Island, New Zealand.
Briggs, Roger M. +5 more
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Various Neogene volcanic rocks associated with calcareous sediments compose the Southern Mountain located from Imogiri at Yogyakarta to Wonogiri at Central Java, Indonesia.
Sri Mulyaningsih +4 more
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Volcanogenic Dark Matter and Mass Extinctions
The passage of the Earth through dense clumps of dark matter, the presence of which are predicted by certain cosmologies, would produce large quantities of heat in the interior of this planet through the capture and subsequent annihilation of dark matter
Afsar Abbas +20 more
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In comparison with previous depictions as well as with coeval and later maps of Naples, Jan van Stinemolen's view (1582) adopts an unusual point of observation by surveying the city from the hillside to the gulf.
Antonino Tranchina
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The rate of volcanism on Venus [PDF]
The maintenance of the global H2SO4 clouds on Venus requires volcanism to replenish the atmospheric SO2 which is continually being removed from the atmosphere by reaction with calcium minerals on the surface of Venus. The first laboratory measurements of
Fegley, Bruce, Jr., Prinn, Ronald G.
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