This paper describes the interactions of a patient and her therapist in the course of psychoanalytic psychotherapy, during which there occurred two significant impasse enactments. At first sight, each resembled a classical impasse. On further review of the case, the interactions took on a different texture that we have described as a pseudo-impasse in the course of the therapy.
View Article and Find Full Text PDFThe mineral composition of 38 human salivary gland stones was described qualitatively on the basis of X-ray diffraction and chemical analysis. In 32 submandibular stones, hydroxyapatite was the most frequently observed phase with a magnesium-substituted whitlockite co-phase (octacalcium phosphate was rarely present). In six parotid gland stones, apatite, magnesium substituted whitlockite and octacalcium phosphate were noted to be the major crystalline phases.
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