18 research outputs found

    An Integrative-Relational Approach in Schizophrenia: From Philosophical Principles to Mentalization-Based Practice

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    In this paper, we explore psychosis and schizophrenia as prototype disturbances, where mentalizing failures are widely seen. We attempt to describe how the process of rekindling mentalizing within attachment relationships (here, the patient-therapist relationship) can have a protective effect not just on the onset of the disturbance, but also when psychosis is already actively installed. We start by discussing mentalizing in training, practice and supervision. We also try to understand it contextually, as a relational concept, within the history of psychological therapies

    Petrology of spinel harzburgite xenoliths from the Kishb Plateau, Saudi Arabia

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    Two spinel harzburgite xenoliths from a Pleistocene alkali basalt unit erupted at the northwestern corner of the Tertiary Kishb Plateau (Saudi Arabia) are characterized by an incipient transition from protogranular to porphyroclastic texture. Vermicular and interstitial spinels are closely associated with neoblasts of olivine, enstatite, and diopside. Sparse exsolution lamellae of high-Ca pyroxene occur in all the enstatite porphyroblasts. Olivine neoblasts are, in many cases, in contact with one another, with the triple grain junctions rarely approaching 120°. Chemical zoning is undetectable by microprobe in spinel and olivine, whereas zoning of Al in enstatite and diopside indicates that chemical equilibrium was not attained. Clear, palegreen glasses occur as veinlets about 10 microns or less in width along grain boundaries and cracks. Consistent counting rates for Na in these glasses were obtained only at 5 kV with a sample current of about 6 namps and counting time of less than 7 s. These glasses are chemically homogeneous and are characterized by relatively high contents of SiO 2 (55.8–58.7 wt%), Na 2 O (6.4–7.6 wt%), and Al 2 O 3 (20.0–21.6 wt%), with inferred volatile contents of less than 1 wt%. The glass is suggested to be of upper mantle origin rather than having developed from the host basalt or by decompressional melting upon ascent.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/47342/1/410_2004_Article_BF00389392.pd
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