Translation

Author(s):  
Graham Shipley

This section of the book contains the English translation of the text. It contains the following sections: Introduction; Europe: Antion to Iapygia; the Adriatic; Epeiros; continuous Hellas; Peloponnese with Crete and southern Cyclades; Macedonia to the Tanaïs; the Black Sea; length of Europe; Asia: Tanaïs to Propontis; Mysia to Kilikia; Cyprus; Syria-Phoenicia to Egypt; length of Asia; Libyē: Non-Carthaginian Libyē; Carthaginian territory; length of Libyē; Beyond the Pillars of Hercules; end matter.

2009 ◽  
Vol 28 (1) ◽  
pp. 57-83 ◽  
Author(s):  
Bruno Soffientino ◽  
Michael Pilson

Count Luigi Ferdinando Marsigli (1658-1730) was a natural scientist and soldier of remarkable and idiosyncratic accomplishment. His first book reported observations and experiments that he carried out during and shortly after his one-year visit to Istanbul during 1679 and 1680. This work is recognized by oceanographers because it contains the first description of a simple laboratory-scale hydrological experiment to show how differences in the density of two water masses lead to two-layer flow. The range of observations and experiments that Marsigli made during that year, however, went well beyond this experiment, and are poorly known: he measured currents using the first example of a paddle-wheel current meter; he determined the water density in the Mediterranean and Black Sea; he estimated the depth of the Bosporus undercurrent; he made detailed meteorological observations and described the effect of weather on current and water levels; he described seasonal migrations of fish to and from the Black Sea, and illustrated the internal anatomy of a mollusk. We present here a complete English translation of Observations and set Marsigli's results in their historical as well as the modern context of the oceanography of the Bosporus region.


1979 ◽  
Vol 40 (C2) ◽  
pp. C2-445-C2-448
Author(s):  
D. Barb ◽  
L. Diamandescu ◽  
M. Morariu ◽  
I. I. Georgescu

Author(s):  
Eleonora P. Radionova

The associations and ecological conditions of the existence of modern diatoms of the North-West (Pridneprovsky), Prikerchensky and Eastern regions of the subtidal zone of the Black Sea are considered. Based on the unity of the composition of the Present and Sarmatian-Meotian diatom flora, an attempt has been made to model some of the ecological c situation of the Late Miocene Euxinian basin.


2002 ◽  
Vol 8 (2-3) ◽  
pp. 231-238
Author(s):  
G.K. Korotaev ◽  
◽  
M.E. Li ◽  
G.A. Tolkachenko ◽  
◽  
...  

2020 ◽  
Vol 42 (4) ◽  
pp. 33-49
Author(s):  
O.V. CHEPIZHKO ◽  
V.V. YANKO ◽  
V.M. KADURIN ◽  
I.M. NAUMKO ◽  
S.M. SHATALIN

For the first time the importance of mineralogical and lithological-petrographical ranks in the line of geological information ranks is substantiated for implementation of long-term forecasts, standard and non-standard approaches to research of physical and geochemical parameters as a basis of creation of complex system of forecast criteria and prospecting indicators of hydrocarbons within the sedimentary cover of Black sea based on the theory of global fluid-flows derivation. These criteria have different sensitivity to the object (hydrocarbon deposits) and are therefore ranked. The ranking determined the following parameters: 1) seismic data within the object, obtained by the method of deep seismic sounding, RWM SDP; 2) parameters of tectono-geodynamic structures; 3) the main characteristics of sedimentary cover and bedrock; 4) geochemical characteristics; 5) parameters of mineral complexes and fluid inclusions in mineral neoformations; 6) the value of the distribution of meiobenthos. Based on modern views of oil and gas geology, structural-tectonic and lithological-facies criteria are among the main ones. The study of the mineralogical component of sediments is made with using mineralogical, thermobarogeochemical and X-ray spectral methods. Fixation of anomalies of fluid flow at the bottom of the Black Sea as to the distribution of abiotic parameters in order to assess the prospects of oil and gas is determined by structural and tectonic features and high permeability of fluid flow; parameters of mineral complexes (minerals, facies) and genetic connections; heterogeneity of geochemical characteristics of bottom sediments; the presence of hydrocarbon inclusions in authigenic minerals of bottom sediments.


Sign in / Sign up

Export Citation Format

Share Document