965 resultados para Russia and transition
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No abstract.
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The Southern Gas Corridor is a system of three complementary gas pipeline projects controlled by Azerbaijan and Turkey, each at a different stage of implementation. The crisis in EU-Russia relations over Ukraine has made the two players interested in the Southern Gas Corridor once again. Brussels views it as an opportunity for a genuine diversification of gas supplies and a way to reinforce its position against Russia. In turn, Moscow’s proposal for Turkey and Greece to join the Turkish Stream gas pipeline project changes the energy map of the regional projects, which indirectly affects the Southern Gas Corridor. This has raised concern in Azerbaijan, which has been making efforts to manoeuvre between the interests of Moscow and Brussels.
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Although the Minsk process brought about a de-escalation of the conflict in Eastern Ukraine, not all of its 13 points have been implemented, including a ceasefire and withdrawal of heavy weaponry. In the absence of a military option, economic sanctions have become the core instrument of the EU and the US, to respond to Russia’s aggression. At the end of June 2016, when EU Heads of State and Government meet to discuss the extension of sanctions against Russia, they should bear in mind that Russia did not implement the commitments it took upon itself in the framework of the Minsk agreements. Given the persistent deadlock in the Ukraine crisis, the leaders of the EU ought to agree to prolong the sanctions against Russia, push for the renegotiation of the Minsk II agreement and widen the ‘Normandy format’ to include the US and bolster reforms in Ukraine.
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DSDP cores from areas of low (Site 505) and high heat flow (Site 504 B) near the Costa Rica Rift, together with seismic profiles from the Panama Basin, have been studied to determine the relationship between: (1) carbonate content and physical and acoustic properties; and (2) carbonate content, carbonate diagenesis and acoustic stratigraphy. Except for ash and chert layers, bulk density correlates strongly and linearly with carbonate content. Velocity is uniform downcore and only small variations at a small scale are measured. Thus an abrupt change in carbonate content will cause abrupt changes in acoustic impedance and should cause reflectors that can be detected acoustically. A comparison of seismic profiler reflection records with physical properties, carbonate content and reflection coefficients indicates that the main reflectors can be identified with ash layers, diagenetic boundaries, and carbonate content variations. Diagenesis of carbonate sediments is present at Site 504B in a 260 m-thick ooze-chalk-limestone/chert sequence. These diagenetic sequences occur in areas of higher heat flow (200 mW/m**2). Seismic profiler records can be used to map the extent and depth of these diagenetic boundaries.
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"First printing."
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Mode of access: Internet.
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Mode of access: Internet.
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Bibliographical footnotes.
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21 cm.
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Mode of access: Internet.
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Mode of access: Internet.
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"May 2009"
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Mode of access: Internet.
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Photocopy.