Study of the Composition of the Fuel Used in a Lamp from an Ancient Settlement from the Taman Peninsula

2020 ◽  
Vol 15 (9-10) ◽  
pp. 623-628
Author(s):  
V. M. Pozhidaev ◽  
Ya. E. Sergeeva ◽  
I. S. Borisevich ◽  
P. K. Kashkarov ◽  
E. B. Yatsishina
Keyword(s):  
Taman Peninsula

GEOECOLOGICAL ASSESSMENT OF DANGEROUS NATURAL PROCESSES DEVELOPMENT FOR THE BLACK AND AZOV SEAS COASTS WITHIN THE TAMAN REGION

2017 ◽  
Author(s):  
Tatiana Podymova ◽  
Tatiana Podymova ◽  
Igor Podymov ◽  
Igor Podymov
Keyword(s):  
Risk Assessment ◽  
Special Consideration ◽  
Taman Peninsula ◽  
Natural Processes

The work is devoted to geoecological assessment of dangerous natural processes development for the Black and Azov seas coasts within the Taman peninsula. Special consideration has given to a factor of tectonic instability for the region. By the example of the events has shown that this factor must stay at first place during geoecological risk assessment.

A hoard of silver coins of the 6th-4th centuries B.C. from the Taman Peninsula

2004 ◽  
Vol 6 (160) ◽  
pp. 27-48
Author(s):  
Mikhail G. Abramzon ◽  
Nina A. Frolova
Keyword(s):  
Taman Peninsula

GEOECOLOGICAL ASSESSMENT OF DANGEROUS NATURAL PROCESSES DEVELOPMENT FOR THE BLACK AND AZOV SEAS COASTS WITHIN THE TAMAN REGION

2017 ◽  
Author(s):  
Tatiana Podymova ◽  
Tatiana Podymova ◽  
Igor Podymov ◽  
Igor Podymov
Keyword(s):  
Risk Assessment ◽  
Special Consideration ◽  
Taman Peninsula ◽  
Natural Processes

The work is devoted to geoecological assessment of dangerous natural processes development for the Black and Azov seas coasts within the Taman peninsula. Special consideration has given to a factor of tectonic instability for the region. By the example of the events has shown that this factor must stay at first place during geoecological risk assessment.

THE DISTRIBUTION OF RADON VOLUMETRIC ACTIVITY ABOVE THE SURFACE OF TAMAN PENINSULA

2017 ◽  
Author(s):  
Tatiana Podymova ◽  
Tatiana Podymova ◽  
Igor Podymov ◽  
Igor Podymov
Keyword(s):  
Coastal Zone ◽  
Decay Energy ◽  
Express Method ◽  
Taman Peninsula ◽  
Secondary Products ◽  
Volumetric Activity ◽  
Field Investigations ◽  
Tectonic Disturbances

The work is devoted to solving the problem of radon mapping of the Taman peninsula as a problem of interaction between the region’s ecosystems and population. An express method of calculating the radon volumetric activity for decay energy of secondary products designed and implemented. Data of the 3-year's field investigations allowed us to plot the map of distribution of radon volumetric activity in the coastal zone of the Azov and Black seas of the Taman Peninsula, as well as over its surface. Some potentially dangerous territory identified. Average values of radon volumetric activity determined in the zones of tectonic disturbances and for the main territory of the Taman.

Recent Tectonic Rupturing on the Mud Volcano of Mount Karabetova, Taman Peninsula

2020 ◽  
Vol 492 (1) ◽  
pp. 361-365
Author(s):  
A. N. Ovsyuchenko ◽  
A. S. Larkov ◽  
A. I. Sysolin ◽  
E. A. Rogozhin ◽  
A. L. Sobisevich ◽  
...  
Keyword(s):  
Mud Volcano ◽  
Taman Peninsula

Underwater mud volcanoes in the Taman Peninsula: Sonar surveys

2016 ◽  
Vol 10 (4) ◽  
pp. 242-247 ◽  
Author(s):  
V. I. Kaevitser ◽  
I. B. Slovtsov ◽  
A. P. Krivtsov ◽  
V. M. Razmanov ◽  
I. V. Smol’yaninov ◽  
...  
Keyword(s):  
Mud Volcanoes ◽  
Taman Peninsula

Archaeological News From the Northern Pontic Region

1995 ◽  
Vol 1 (1) ◽  
pp. 3-39 ◽  
Author(s):  
Michail Yu. Treister
Keyword(s):  
Rural Settlements ◽  
Taman Peninsula ◽  
Classical Archaeology ◽  
The North ◽  
North Western ◽  
Language Literature

AbstractThis article gives a picture of developments in the Classical archaeology of the Northern Pontic region in the 1980's, surveying (Russian- and Ukrainian-language) literature, excavations and finds. The areas and sites covered include the Lower Dniester basin: Tyras, Nikonion, the Kosharskoye settlement, the island of Leuke; Olbia and its chora; Berezan (and its necropolis); the North-Western Crimea: Kalos Limen, Kerkinitis; the Western Crimea: Chersonesus and its Chora (incl. the Heraclean peninsula); Bosporus: Pantikapaion, Iluraton, the rural settlements ; the Lower Don Area: the Taganrog settlement, Tanais, the Elisavetovskoye fortified settlement; the Taman peninsula and the lower Kuban: Kepoi, Phanagoria, Hermonassa, Gorgippia and its chora.

scholarly journals Bacteria of the Clostridium Genus, Methane and Hydrogen Sulfide in Sulfide Mud of the Taman Peninsula Reservoirs

2018 ◽  
Vol 18 (3) ◽  
pp. 315-322 ◽  
Author(s):  
Yury Aleksandrovich Fedorov ◽  
Gar'kusha Dmitry Nikolayevich ◽  
Roman Gennad'yevich Trubnik
Keyword(s):  
Hydrogen Sulfide ◽  
Taman Peninsula

scholarly journals Neotectonics of the Pleistocene deposits in the northeast of Taman peninsula, the southern Asov sea region

2019 ◽  
pp. 12-35
Author(s):  
A. S. Tesakov ◽  
O. V. Guydalenok ◽  
S. A. Sokolov ◽  
P. D. Frolov ◽  
V. G. Trifonov ◽  
...  
Keyword(s):  
Developmental Stages ◽  
Taman Peninsula ◽  
Matuyama Chron ◽  
Mud Volcanism ◽  
North Eastern ◽  
Quaternary Deformation ◽  
Reversed Polarity ◽  
Definition Of ◽  
Middle Member ◽  
North Eastern Part

Studies in paleomagnetism, structural geology, and paleontology (mammals, molluscs, palynology) in the coastal sections of the Taman Peninsula north-eastern part (2017–18) resulted in definition of three sedimentary members. The sandy and clayey lower member (I) formed at 2.1–1.7 Ma. It contains a normally magnetised zone within deposits of reversed polarity correlated to the Olduvai Subchron and the Matuyama Chron. The middle member (II) is composed of the basal pebbles overlain by sands. The reversely magnetised deposits hosting the Sinyaya Balka site, the type locality of the Tamanian faunal complex, is correlated to the basal bed of the middle member II. The overlying sands are normally magnetised (Jaramillo Subchron) in the lower part and show reverse polarity (late Matuyama Chron) in the upper part. The member II is dated in the range of 1.3–0.78 Ma. The silty upper member (III) represents Middle-Late Pleistocene. The dissimilar displacement degree of the members reflect developmental stages of the Quaternary deformation. The member I is characterised by dip angles up to 70° is fragmented by faults into blocks. The member II filled the relief of the eroded surface of the Member I and also displaced by faults. The faulting separated the bone-bearing body of the Taman faunal complex as a rock land-slide. The attitude of the member III outline an anticline with a gentle south-western and a steeper north-eastern limbs eroded by land-slides and marine abrasion. During its entire life the anticline was affected by mud volcanism. The anticline continues its development at the present stage.

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