MESSINIAN PALEOENVIRONMENTAL CHANGES IN THE EASTERNMOST MEDITERRANEAN BASIN: ADANA BASIN, SOUTHERN TURKEY

This sedimentological and sequence-stratigraphic study focuses on the late Miocene deposits in one of the largest periMediterranean basins of southern Turkey, the Adana Basin, which formed as a Tauride foreland depression accumulating molasse deposits. The Tortonian–Messinian shallow-marine Handere[r]

High flood 1663.70 1238.20 48.87 2950.77
Medium flood 1653.20 1227.20 46.87 2927.27
Generally, in the future, if there would be only Dau Tieng reservoir used in flood control, the ability to reduce flood in the downstream would[r]

The Sivas Cenozoic Basin and coeval Central Anatolian basins such as Çankırı and Tuz Gölü are characterized by both marine and terrestrial sediments ranging in age from the Eocene to early Miocene. The evaporite regime here generally appeared during the late stage of Eocene transgression and persist[r]

What geologists call the Basin and Range Province in the United States roughly coincides in its northern portions with the geographic province known as the Great basin.. The Great Basin[r]

The geology of the Çankırı Basin has been studied using multi-source data including satellite images, aerial photos, gravimetric data and seismic sections, which are subsequently used to generate maps and a 3D model of that part of the basin covered by the seismic sections.

Recently, surface water of the Dong Nai river basin has been influenced by socio-economic development activities, so river water quality is reduced. The author used a number of methods such as collecting data, processing data, analyzing systems, and chart - map to assess water quality in the Dong Na[r]

a degree in finance, Marty has built more than 40 multifamily apart- ment buildings, managed more that 1,000 units, and written and lec- tured extensively about all areas related to real estate investing over the past 30 years. He is also the managing broker of Buckingham Real E[r]

contamination by prolonged flooding; destruction by sudden violent events such as landslides; and inundation by sea level rise storm surges. Similar to above, we are discussing an amplification of historical events and associated damages that already impact the LMB’s stock of rural infrastr[r]

Another example of fisheries management in the Mekong is the fishing lot system used in Cambodia. This system is very effective in galvanising users to protect the resource. Because the government earns revenue from the system, it has an increa[r]

Fingerprinting petroleum pollutants in the mediterranean sea Fingerprinting petroleum pollutants in the mediterranean sea Fingerprinting petroleum pollutants in the mediterranean sea Fingerprinting petroleum pollutants in the mediterranean sea Fingerprinting petroleum pollutants in the mediterranean[r]

However, tree mortality may result from multiple factors, including human activity, fire suppression, competition, insect infestation, or a combination of these disturbances [22, 45]. Prior to 1950, the Xilin River Basin was still a virgin territory, implying that no direct relationshi[r]

Thereby, the calculation results clearly factors C are the areas with poor vegetation cover, bare areas – concentrated downstream of the river basin in Sapa the index [r]

The research results show that the vulnerability index of the Dong Nai River basin in the province of Lam Dong is also spatially differentiated and in general, the value of the vulnerability index is at a moderate level (VI = 0.23). It is observed that the Vulnerability Index for the Dong Nai - Lam[r]

The North Anatolian Fault System (NAFS) that separates the Eurasian plate in the north from the Anatolian microplate in the south is an intracontinental transform plate boundary. Its course makes a northward convex archshaped pattern by flexure in its central part between Ladik in the east and Kargı[r]

Rapid increase in activities like urbanization, socioeconomic activities and environmental changes are responsible for land use/land cover changes (LULCC). Hence, it is important to know LULCC to determine its impacts on hydrology. In this study an attempt has been made to analyze LULCC in the Koyna[r]

The Karaçayır kaolinite deposit, situated in the Uşak-Güre basin of western Turkey, is hosted by rhyolite and andesite of the Miocene Dikendere volcanics, and by muscovite schist, glaucophane schist, talc schist and chlorite schist of the Palaeozoic Eşme Formation.

This paper focuses on relative fluctuation of sea water temperatures during the Middle and Late Miocene, emphasised by cold and warm nannofossil changes in abundance in 2 wells. At the A-1 well in the Middle Miocene, the total abundance of cooler water species is 45%, while that of the warmer specie[r]

occurred over the whole sea area, only along the northeastern and eastern coast of the sea did enormous salt strips up to 100 km wide appear; storms, however, occurred over the whole sea wherever the dried seabed was exposed. Light- weight particles rose to a hei[r]

3. These days food .................................... more and more expensive. 4. The world ................................ Things never stay the same.
5. The cost of living ..................................... Every year things are dearer.
6. George has gone to work <[r]

İzmir Bay is an actively growing shallow marine basin controlled by active faults trending NE, NW, N–S and E–W, in the West Anatolian Extensional Province. The bay of İzmir is a lazy L-shaped superimposed basin which is topographically divided into an E–W-trending inner bay and a NW-trending outer b[r]