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We have used field-based structural analyses and geological mapping in five key ophiolite massifs (Luobusa, Zedang, Xigaze, Jiding and Dongbo) and petrofabric studies of core samples recovered through the Luobusa Scientific Drilling Project to document the structural architecture and the deformation history of the ITSZ.
Similar modifications of magnetic properties have been reported in studies of core samples from lake sediments in various regions (e.g., Anderson and Rippey 1988; Snowball 1993; Nowaczyk et al. 2001).
In the same region, studies of geomagnetic field models identified formation of flux patches (Jackson et al. 2000; Finlay and Jackson 2003) and studies of core flow models reported strong poloidal flows (e.g., Amit and Pais 2013; Baerenzung et al. 2016).
The research objectives assigned to the mission are: (a) studies of core dynamics, geodynamo processes, and core-mantle interaction; (b) mapping of the lithospheric magnetisation and its geological interpretation; (c) determination of the 3-D electrical conductivity of the mantle; and (d) investigation of electric currents flowing in the magnetosphere and ionosphere.
In the light of recent perception from palaeomagnetic records, indicating surprisingly fast magnetic field reversals (Nowaczyk et al., 2012), and in view of the fast evolution of the field revealed by CHAMP satellite data (Lesur et al., 2008), it is important to pursue data collection, which is foundation for global studies of core dynamics and core-mantle interaction.
Multiproxy studies of core MD95-2042 [37]–[43] and MD04-2845 [44] have documented the impact of the Dansgaard-Oeschger millennial-scale climatic variability and Heinrich Stadials (HSs) in the mid-latitudes of the eastern North Atlantic Ocean and Western Europe.
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Integrated ichnologic, sedimentologic, and stratigraphic studies of cores and well logs from Lower Pennsylvanian oil and gas reservoirs (lower Morrow Sandstone, southwest Kansas) allow distinction between fluvio-estuarine and open marine deposits in the Gentzler and Arroyo fields.
In this research, SVM classification method is used to lithology prediction from inverted seismic attributes data and petrophysical logs based on petrographic studies of cores lithology in a heterogeneous carbonate reservoir in Iran.
It is the de-facto standard in many astrophysical simulations and in particular in studies of core-collapse supernovae (CCSN).
In the present study, phospho-tau concentrations in the extensions were numerically lower than in the core studies, irrespective of core study treatment.
Students in the Business M.A. concentration are steeped in money and enterprise through the study of core subjects including accounting, corporate finance, economic theory and securities.
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