14 research outputs found

    Hemoperfusion Treatment Of Digital Intoxication In Chronic Hemodialysis Patient

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    Diagnosis of Digitalis intoxication depends on good history taking, clinical signs and symptoms, and digoxin level. Sixty one years old female with diabetes mellitus (DM), coronary artery disease (CAD) and end-stage renal failure administered to emergency department with complaints of dyspnea and chest pain. Digoxin 0.50 mg once a day was prescribed by an internal medicine physician and she has been taking the drug for 7 days. In our case digoxin level was decreased to valuable level after hemoperfusion. In conclusion it was observed that hemoperfusion therapy of digitalis intoxication in chronic hemodialysis patient is effective

    Evolution Of Camlik Fissure-Ridge Travertines In The Baskale Basin (Van, Eastern Anatolia)

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    Fissure-ridge travertines (FRTs) are of great importance for the determination and comparison of tectonic deformation in a region. The coeval development of these travertines with active fault zones supplies significant information about regional dynamics in terms of deformation pattern and evolution. In this paper, the characteristics of FRTs of the Baskale basin (eastern Turkey) and responsible regional tectonism are discussed for the first time. The Baskale basin is located between the Baskale Fault Zone (BFZ) characterised by Camlik fault and Isikli-Ziranis fault. It is located between dextral Yuksekova Fault Zone and southern end of dextral Guilato-Siahcheshmeh-Khoy Fault system (Iran). Various morphological features indicating recent activity are exposed along the BFZ, including offsetting rivers, fissure-ridge travertine and fault scarps. The Camlik fissure-ridge travertine composing of three different depositions is observed along the eastern edge of the BFZ with approximately parallel orientations. The Famlik fissure-ridge travertine has been formed and developed on fault zone related to strike-slip or oblique movements. We explain how kinematic changes of faults can influence the fissure-ridge development.WoSScopu
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