The Deep Roots of Geology: Tectonic History of Australia and its Margins expressed by Mantle Anisotropy [PDF]
Caroline Eakin
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Introduction Geological background Ophiolites have played a major role in our understanding of Earth’s processes ranging from seafloor spreading, melt evolution and magma transport in oceanic spreading centers, and hydrothermal alteration and ...
Farhad Ghaseminejad, Ghodrat Torabi
doaj
Report on workshop"Structure and evolution of Eurasia (super-) continent"
A workshop on Structure and evolution of Eurasia (super-) continent" was held on 23rd February 2004, at the National Institute of Polar Research with 29 participants.
Masaki Kanao
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The relationship between the Proto‐Tethys and Paleo‐Tethys is still debated. Some researchers believe that the Paleo‐Tethys opened after the Proto‐Tethys closed, while others argue that they are the same ocean with two stages of subduction.
Rutao Zang +6 more
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Significance and Petrochemistry of Upper Mantle–mantle Transition Zone Metaperidotites and Oceanic Crust Metagabbros within the Kazdağı Metaophiolite: Implications for the Geological Evolution of the Izmir–Ankara–Erzincan Ocean, Northwestern Turkey [PDF]
Ender Sarıfakıoğlu +3 more
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Geological records of transient fluid drainage into the shallow mantle wedge
Kazuki Yoshida +5 more
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The closure of the Vardar ocean (the western domain of the northern Neotethys) from early Middle Jurassic to Paleocene time, based on surface geology of eastern Pelagonia and the Vardar zone, biostratigraphy, and seismic-tomographic images of the mantle below the Central Hellenides [PDF]
Rudolph Scherreiks +1 more
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Length of day variations due to mantle dynamics at geological timescale [PDF]
M. Greff‐Lefftz
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The Deep Roots of Geology: Tectonic History of Australia as expressed by Mantle Anisotropy 
Caroline Eakin
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