Expedition 396 Preliminary Report : Mid-Norwegian Margin Magmatism and Paleoclimate Implications

Publisher PD

Secure direct communication using Einstein-Podolsky-Rosen pairs and teleportation

A novel scheme for secure direct communication between Alice and Bob is proposed, where there is no need for establishing a shared secret key. The communication is based on Einstein-Podolsky-Rosen pairs and teleportation between Alice and Bob. After insuring the security of the quantum channel (EPR pairs), Bob encodes the secret message directly on a sequence of particle states and transmits them to Alice by teleportation. In this scheme teleportation transmits Bob's message without revealing any information to a potential eavesdropper. Alice can read out the encoded messages directly by the measurement on her qubits. Because there is not a transmission of the qubit which carry the secret message between Alice and Bob, it is completely secure for direct secret communication if perfect quantum channel is used

Mid-Norwegian Margin Magmatism and Paleoclimate Implications: Expedition 396 Preliminary Report

The opening of the North Atlantic about 56 My ago was associated with the emplacement of the North Atlantic Igneous Province, including the deposition of voluminous extrusive basaltic successions and intrusion of magma into the surrounding sedimentary basins. The mid-Norwegian Margin is a global type example of such volcanic rifted margins and is well suited for scientific drilling with its thin sediment cover and good data coverage. During International Ocean Discovery Program Expedition 396, 21 boreholes were drilled at 10 sites in five different geological settings on this volcanic margin. The boreholes sampled a multitude of igneous and sedimentary settings ranging from lava flow fields to hydrothermal vent complexes, along with thick successions of upper Paleocene and lower Eocene strata. A comprehensive suite of wireline logs was collected in eight boreholes. The main goals of the expedition were to provide constraints for geodynamic models to test different hypotheses that can explain the rapid emplacement of large igneous provinces and the hypothesis that the associated Paleocene/Eocene Thermal Maximum was caused by hydrothermal release of carbon in response to magmatic intrusions. Successful drilling, combined with high core recovery of target intervals of all nine primary sites and one additional alternate site, should allow us to achieve these goals during postcruise work

Geo. A. O'Brien

35-1ClaimsOn the Relief of G. O'Brien. [966] Clerk for the Chickasaws during 1845-1846; Chickasaw fund.1858-10

L'anse and Vieux De Sert Bands of Chippewa Indians

43-1Indian AffairsReport on the L'Anse and Vieux de Sert Bands of Chippewas. [1624] Had lands given them under the treaty of 30 Sept. 1854 wrongfully withheld.1874-13

Memòria Digital de Catalunya

Inclou (f. r6): Ex Marcellino Graeco Thvcydidis Atheniensis vita Bartholomeo Parthenio Benacensi interpreteEl traductor és Lorenzo Valla (f. a2)Títol obtingut de l'epígrafEls f. a1 i r8 blancs, signatures: a-r8Registre al darrer f.Espais buits per a inicial

Guy Carpenter

29-1ClaimsReport : Petition of G. Carpenter. [489] Black Hawk war; 1832; Michigan militia.1846-6

amplexicaulis

Bear River, Uint

bursa-pastoris

Capsella bursa-pastoris (L.) Medie.Shepherd's PurseBourse de bergerGwen WalkerAnnual or winter annual spreading only by seeds. A very common weed, occuring in wastelands and cultivated areas. Introduced from Europe before 1700. Collected by the experimental greenhouses, Provincial Horticulture Station, Brooks, Alberta

bursa-pastoris

Capsella bursa-pastoris (L.) Medie.Shepherd's PurseBourse de bergerAHRC, Plot 14Peggy Morto