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| 1 | Assessing land-use and land-cover changes in relation to geographic factors and urban planning in the metropolitan area of ConcepciSn (Chile): implications for biodiversity conservation显示文摘 | CAROLINA R JOAN P CORINA B | 2013 | Applied Geography2013，39，： | 1 |
| 2 | Fe2O3-TiO2 thin films prepared by sol-gel method 显示文摘 | Suciu R C Corina R M Silipas T D | 2011 | Environmental Engineering and Management Journal2011，10，2： | 1 |
| 3 | Impact of body tilt on the central aortic pressure pulse显示文摘 | Corina R Lucas L Bemard W | 2015 | Physiological Reports2015，3，4： | 1 |
| 4 | Airborne p-band SAR applied to the aboveground biomass studies in the Brazilian tropical rainforest显示文摘 | Joao R Santos Corina C Freitas Lucian S Araujo | 2003 | Remote Sensing of Environment2003，87，： | 1 |
| 5 | Dissociation of action and object naming:evidence from cortical stimulation mapping显示文摘 | Corina DP Gibson EK Martin R | | 0，，01： | 1 |
| 6 | Petrology of ultramafic to mafic cumulate rocks from the G?ksun(Kahramanmaras) ophiolite,southeast Turkey显示文摘The G?ksun(Kahramanmaras)ophiolite(GKO),cropping out in a tectonic window bounded by the Malatya metamorphic unit on both the north and south,is located in the EW-trending lower nappe zone of the southeast Anatolian orogenic belt(Turkey).It exhibits a complete oceanic lithospheric section and overlies the Middle Eocene Maden Group/Complex with a tectonic contact at its base.The ophiolitic rocks and the tectonically overlying Malatya metamorphic(continental)unit were intruded by I-type calc-alkaline Late Cretaceous granitoid(~81-84 Ma).The ultramafic to cumulates in the GKO are represented by wehrlite,plagioclase wehrlite,olivine gabbro and gabbro.The crystallization order for the cumulate rocks is as follows:olivine±chromian spinel→clinopyroxene→plagioclase.The major and trace element geochemistry as well as the mineral chemistry of the ultramafic to mafic cumulate rocks suggest that the primary magma generating the GKO is compositionally similar to that observed in the modern island-arc tholeiitic sequences.The mineral chemistry of the ultramafic to mafic cumulates indicates that they were derived from a mantle source that was previously depleted by earlier partial melting events.The highly magnesian olivine(Fo77-83),clinopyroxene(Mg#of 82-90)and the highly Ca-plagioclase(An81-89)exhibit a close similarity to those,which formed in a supra-subduction zone(SSZ)setting.The field and the geochemical evidence suggest that the GKO formed as part of a much larger sheet of oceanic lithosphere,which accreted to the base of the Tauride active continental margin,including the ispendere,K?mürhan and the Guleman ophiolites.The latter were contemporaneous and genetically/tectonically related within the same SSZ setting during the closure of the Neotethyan oceanic basin(Berit Ocean)between the Taurides to the north and the Bitlis-Pütürge massif to the south during the Late Cretaceous. | Osman Parlak Utku Bagcı Tamer Rızaoglu Corina Ionescu GüzideÖnal Volker Höck Hüseyin Kozlu | 2020 | Geoscience Frontiers2020，11，1： | 0 |
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