Physical properties of seafloor sediments from the Russian Pechora Sea /
(1 983), corresponds to the top of the Boulder Clay.
| Main Author: | |
|---|---|
| Format: | Thesis eBook |
| Language: | English |
| Published: |
[Place of publication not identified] :
[publisher not identified] ;
1996.
|
| Subjects: | |
| Online Access: | Link to OAKTrust copy |
| Summary: | (1 983), corresponds to the top of the Boulder Clay. (TOC). The medium to coarse silt range is associated with 28 surficial samples in the Pechora Sea indicate a close a thickness between 0 and 1 0 meters of the most recent above properties show the density profiles as sensitive and, and correlated with their corresponding lithological units and geotechnical properties of the surficial marine sediments and x-radiographs records. Furthermore, measurements of the Arguments support the glacial nature of Boulder Clay deposits within the study area, solving the long consequently, better indicators of lithological changes controversy correlation between mean grain size and Total Organic Content corresponding stratigraphic sections indicate that the deposits or crops out in small promontories as a hard bottom directional flow is responsible for the formation of the downcore than the velocity profiles; conversely, the presence Furthermore, this reflector is either covered conformably by geophysical data and in the Pechora Sea. Profiles of bulk density, porosity, in the sea floor. The results of the grain size analysis of Koshki Islands. modified paleogeographical maps. Interpretation of high of large clasts and shell fragments are better indicated gn of the dynamic influence of the longshore current whose east outside of the Pechora Gulf, exhibit well sorting as a result Pechora area. An evaluation of the influence of the Novaya Pechora Sea and Pleistocene deposits in the regarding the marine or glacial origin for these late regional seismic reflector Rl, called after Epshteyn et al. resolution seismic profiles and the correlation with their Russkiy Zavarot Peninsula and the Ostrava Gulyayevskiye sands shows TOC values lower than 0.5%. These sands, located Scandinavian ice masses on the convergence character of the that characterizes and quantifies the physical, acoustical, the direction of the ice flow are presented and supported by the velocity profiles. Sedimentological and geophysical This study is the first of its kind in the English language TOC values larger than 0.5%; th6 range of fine to very fine velocity, and shear strength for seven cores are presented Zemlya and |
|---|---|
| Item Description: | "Major subject: Oceanography". Vita. |
| Physical Description: | x, 78 leaves : illustrations, maps ; 28 cm. Also available online. Issued also on microfiche from Lange Micrographics. |
| Bibliography: | Includes bibliographical references. |