Do you want to publish a course? Click here

Biostratigraphical study of Middle Miocene deposits in Northern part of Al-Kapeer Al-Shemaly

دراسة بيوستراتغرافية لتوضعات الميوسين الأوسط في الجزء الشمالي من حوض نهر الكبير الشمالي

906   0   19   0 ( 0 )
 Publication date 2016
  fields Geology
and research's language is العربية
 Created by Shamra Editor




Ask ChatGPT about the research

Middle Miocene deposits reveal the form of outcrops which are limited in area on the northern boards of the basin of AL-KABEER Al-Shemaly River. It is characterized by a large and fast changes in thickness and facies. This study focused on the results of careful Fossile analysis of 41 samples (hard and soft) which were taken from the three geological sections, through which the principal zones, which characterize middle Miocene, were confirmed depending on planktonic foraminifera. N9, -Orbulina suturalis-Globerotalia peripheroronda N10-N13-Globerotalia fohsi, Sphaaerodinellopsis subdehiscens- Globigrina drury , N14 – Globigerina nepenthes- Globerotalia siakensis. It was identified as benthic foraminifera, which has been characterized by its diversity and their increasing numbers in the northern boards of the Neogene basin and identify the lithology of these deposits consisting of alternations of limestone and limestone of medium hardness to very soft marl with different colors. This study also contributed to the detection of some paleogeographical development in the basin in that period of time.

References used
Beard, J.H.& Jeefords, P. M., Cenozouc Planktonic foraminifera zonation and charaste Ristics of index formis. USA., univ. Kansan, AR. 62, 1975, P.245-330, P. 78-79
Cokopov, B. C. &Gamouda, A. E, practis ,index microfauna of foraminifera Mezozouc, Leningrad, 1991, P.225-373
Deubert. L., Liban, Syria et bordure des pays voisins: Notes et Mem, Moyenorient, 1966,V8, P.251-358
rate research

Read More

Study of the general characteristics of Fractures in the central part of the AL-Kabir AL- Shimali river basin showed the presence of several main groups of Fractures with directions NE-SW _ NNESSW, NW-SE , E-W.and showed increased fracture rate in the northern and southern parts of the study area, and that the spacing between the Fractures close to the medium convergence (5-34) cm , also show a aperture ranged between (0.1-5.1) cm, where aperture width was increased in southwest of Lake 16 October near Lattakia- Kless fault .
The lithological study and micropaleontological analyses of 21 samples taken from four geological sections of lower Miocene deposits led to a stratigraphic study for determination of enrichment of planktonic species in these deposits . These speci es were combined with biozones of lower miocene and their stratigraphic distribution in the studied sections according to planktonic foraminifera of worldwide spreading . This study contributed in understanding of paleogeographic development of Neogene basin within this period of time , which appeared as a marine progress in lower Miocene , which continued up to upper Miocene in the northwestern part of Syria . The sediments of lower Miocene consisted of marl , clay marl deposits with interfacial layers of clay and limestones or marl limestones deposited unconformithy with nummoliticlimestones of Eocene , or cretaceous carbonates rich in betome sometimes .
The aim of this research is to identified the tectonic evolution of Naher Al-Kabir Al-Shimaly Basin from tectonic subsidence curve witch calculated from Lattakia1 well data. Tectonic subsidence was identified in lower-middle Jurassic en relation o f opening of East Mediterranean basin. A subsidence is occurred in Cenomaniane, after a stage of uplift in late Jurassic-lower Cretaceous en relation to fold and erosion known at regional scale.
This study deals with the determination of total mercury concentration in the water taken from three sites on Al-Kabeer Al-Shemaly River ( near the industrial area and Al- Damat Lake, and 16 Tishreen Lake), also the effect of some physio-chemical p arameters including: DO, pH, T °C. of water in the three sites was studied. Results showed that the total mercury concentration was low in general, where the medium concentration in the three studied sites was 0.29 ppb and it was less than the permission level of total mercury in the surface water(> 10 ppb), the higher value of the medium concentration of total mercury(0.35, 0.31, 0.21)ppb was recorded in the Industrial Area, Damat Lake, then 16 Tishreen Lake, respectively. For the changes in the total concentration of mercury in the three studied sites during seasons of a year, was higher in Summer comparing with other seasons. The results showed positive correlation coefficient between the total mercury concentration and temperature, pH value, but it was negative with DO in Summer.
Al-Kabeer Al-Shemale river rises from Aqraa Mountain and coastal mountains, it is considered one of the largest rivers in the coastal area.Its catchment area is 1097 km2, and empties into the sea to the southern of Lattakia.The study aims to determin e the impact of climate change on the river discharge. Since the rainfall is the major factor in the runoff formation in the river catchment, the rainfall changes have been studied in climatic stations located within the catchment and its surroundings, and for a period of time exceeding thirty years. The study found that the general trend of rainfall change and runoff with time is decreasing, declining rainfall values ranged in the studied stations between (0.4-12.5) mm per year, and the runoff reached 0.08m3/s in the year. A mathematical equation, predict river discharge after knowing the values of daily precipitation, has been concluded.
comments
Fetching comments Fetching comments
Sign in to be able to follow your search criteria
mircosoft-partner

هل ترغب بارسال اشعارات عن اخر التحديثات في شمرا-اكاديميا