944 resultados para Northern leopard frog


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Health Technical Memorandum 82 Alarm and detection systems Supplement A: Automatic fire control systems and voice alarm systems

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Health Technical Memorandum 82 Alarm and detection systems Supplement A: Automatic fire control systems and voice alarm systems

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Practice Note 10 Laboratories on Hospital Premises

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Practice Note 4 Hospital Main Kitchens

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Northern Ireland Fire Technical Memorandum 81 Fire precautions in new healthcare premises

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Practice Note 11 Reducing unwanted fire signals in healthcare premises

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Practice Note 7 Fire Precautions in patient hotels

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Practice Note 6 The prevention and control of wilful fire raising in healthcare premises

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Practice Note 5 Commercial enterprises on hospital premises

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Practice Note 3 Escape bed lifts

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Practice Note 2 Policy and Principles

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A Model Management Structure for Fire Safety

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The Northern Ireland Action Plan for Learning Disability Nursing

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The Northern Snake Range (Nevada) represents a spectacular example of a metamorphic core complex and exposes a complete section from the mylonitic footwall into the hanging wall of a fossil detachment system. Paired geochronological and stable isotopic data of mylonitic quartzite within the detachment footwall reveal that ductile deformation and infiltration of meteoric fluids occurred between 27 and 23 Ma. Ar-40/Ar-39 ages display complex recrystallization-cooling relationships but decrease systematically from 26.9 +/- 0.2 Ma at the top to 21.3 +/- 0.2 Ma at the bottom of footwall mylonite. Hydrogen isotope (delta D) values in white mica are very low (-150 to -145 %) within the top 80-90 m of detachment footwall, in contrast to values obtained from the deeper part of the section where values range from -77 to -64 %, suggesting that time-integrated interaction between rock and meteoric fluid was restricted to the uppermost part of the mylonitic footwall. Pervasive mica-water hydrogen isotope exchange is difficult to reconcile with models of Ar-40 loss during mylonitization solely by volume diffusion. Rather, we interpret the Ar-40/Ar-39 ages of white mica with low-delta D values to date syn-mylonitic hydrogen and argon isotope exchange, and we conclude that the hydrothermal system of the Northern Snake Range was active during late Oligocene (27-23 Ma) and has been exhumed by the combined effects of ductile strain, extensional detachment faulting, and erosion.