English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Mineralogical investigations of the coarse-silt fraction (0.1-0.05 mm) were carried out on samples obtained from Holes 379A, 380, 380A, and 381 (DSDP Leg 42B) with the purpose of determining the source areas of terrigenous material and peculiarities of its distribution in the Black Sea during late Cenozoic time. The coarse-silt fraction was divided into heavy and light subfractions using bromoform (sp. gr.>2.9). Mineralogical analyses were made on immersion slides under polarizing microscope MIN-8, using no less than 300 grains per slide. The composition of samples studied is given in Tables 1 to 4. Holocene and late Pleistocene deposits in adjacent drilling areas (Figure 1, see also Fig. la in Trimonis and Shimkus, this volume), which were studied earlier, are shown in Table 5.

Mineral Composition of Coarse-Silt Fraction of the Black Sea Late Cenozoic Sediments