The Achemmach region is located 40 km to the SW from Meknes city and 6 NE frm Hammam mine. It part of Paleozoic massif Central Morocco. studied area formed by two rock-types: (i) a meta-sedimentary sequence composed Middle Visean limestone shale-sandstone withflyschoid Upper Visean-Namurian age, (ii) magmatic rock series represented volcanic rocks (pillow-lavas), hypovolcanic (dolerites) olivin...

Heat is generated during the exothermic reaction associated with plaster splint application. The amount of heat generated is affected by the plaster thickness, dipping water temperature, and extremity elevation method. The authors assessed the effect of these variables on skin and plaster temperatures. Short-leg posterior splints were applied to noninjured extremities on a volunteer using 2 pro...

Objectives This research was intended to provide a greater understanding of the context and needs of aged care seating, specifically:To conduct an audit of typical chairs used in aged care facilities;To collect data about resident and staff experiences and behaviour around chairs in order to gain a deeper understanding of the exact issues that residents and staff have with the chairs they use a...

The Upper Cretaceous Ganj complex, a part of the Jazmurian ophiolitic belt, is located on the western boundary of Jazmurian depression and separated from Kahnuj ophiolitic complex by north-south trending Jiroft fault. The complex consists of lava flows, pillow lavas, acidic plutonic and sedimentary rocks which are intruded by northwest-southeast trending dykes. It does not resemble a classical ...

the upper cretaceous ganj complex, a part of the jazmurian ophiolitic belt, is located on the western boundary of jazmurian depression and separated from kahnuj ophiolitic complex by north-south trending jiroft fault. the complex consists of lava flows, pillow lavas, acidic plutonic and sedimentary rocks which are intruded by northwest-southeast trending dykes. it does not resemble a classical ...

The Nazca Ridge (NR) was formed near the interaction of a hotspot mantle plume and an active spreading center. We use active-source wide-angle seismic data to obtain 2-D Vp Vs tomographic models, hence Poisson's ratio (?) structure beneath NR. Results show ?2 km thick layer 2A with ? values 0.25–0.32 in uppermost crust interpreted as pillow basalts low degree fracturing and/or hydrothermal alte...