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21	Självtranscendens : upplevelse, utveckling och psykologiska förändringar / Selftranscendence : experience, development and psychological changes Friman, Henrik January 2014 (has links) Psykologiska processer där identifikationen med jaget och medvetandets innehåll upphör kan tänkas utgöra en hälsosam motvikt i dagens samhällskultur där centrering kring jaget, stress, depression och meningsförlust, ofta förekommer. Självtranscendens har beskrivits som en expansion av medvetandet och en rörelse bortom gränserna för ens självmedvetenhet och självuppfattning, antingen tillfälligtvis eller som en relativt stabil perspektivförändring som utvecklats under livsloppet. Sex personer mellan 54 och 100 år med erfarenhet av självtranscendenta perspektiv intervjuades i studien i syfte att induktivt generera mer kunskap om hur självtranscendens kunde upplevas, utvecklas och förändra en människas perspektiv. Genom en tematisk analys framkom att en regelbunden aktivering av självtranscendenta medvetandetillstånd särskilt inverkade på utvecklingen och kopplades till principer om neuroplasticitet. Självtranscendensutvecklingen medförde även förändringar i respondenternas perception av inre och yttre fenomen exempelvis vad gäller känslighet, jagupplevelse och möjlighet till distans och objektivitet, vilket även bidrog till psykologisk hälsa. självtranscendens utveckling upplevelse psykologiska förändringar neuroplasticitet jaget peakupplevelse höjdpunktsupplevelse flow platå-upplevelse gerotranscendens transcendens meditation mindfulness ACT yoga självupplevelse personlighetsdrag Maslow Tornstam Cloninger Reed kvalitativ studie tematisk analys buddhism humanistisk psykologi transpersonell psykologi Wilber Wade självförverkligande psykologisk utveckling utvecklingspsykologi självförverkligande motivation drivkraft perception förändringar i perception känslighet objektivitet distans decentrering jagupplevelse självbild självmedvetenhet Psychology Psykologi
22	DETRITAL RECORD OF PALEOZOIC AND MESOZOIC TECTONICS OF THE NORTHWESTERN CORDILLERAN MARGIN: A CENTRAL ALASKAN PERSPECTIVE Lukas Geiger-Rigby McCreary (18824572) 14 June 2024 (has links) <p dir="ltr">The Intermontane terranes represent one of the largest composite accreted terranes that built the northern Cordillera. To better understand the interactions between the continental margin of Laurentia and the Intermontane terranes, this study analyzes twelve detrital zircon samples (n=3232) from a Neoproterozoic (?) to Cretaceous metasedimentary stratigraphic section exposed in central Alaska. Distinct detrital zircon populations have been identified and are interpreted to represent four stages in the geologic development of this part of western North America. Stage 1 extends from the Neoproterozoic (?) to the Early Paleozoic, and is characterized by Proterozoic and Archean detrital zircon populations that correlate with Laurentian sources of sediment. We interpret Stage 1 to represent deposition along the northwestern continental margin of Laurentia. Stage 2 extends from the Silurian (?) to the Devonian and is characterized by a dominant Devonian and Silurian detrital zircon population. We interpret Stage 2 to have been deposited in a backarc basin coeval with active volcanism as the Yukon-Tanana terrane was rifted away from the Laurentian continental margin as the Slide Mountain Ocean opened. Stage 3 extends from the Mississippian to the Jurassic and records a shift back to sediment sources with abundant Proterozoic and Archean zircon. We interpret this stage to represent deposition of Laurentian detritus along the eastern margin of the Slide Mountain Ocean basin. Stage 4 is represented by the Lower Cretaceous strata of the Manley basin that contain one major Late Triassic to Early Jurassic detrital zircon population. We interpret this population to be sourced from the syn-collisional and post-collisional Late Triassic to Early Jurassic plutons and related sedimentary basins of the Intermontane terranes that were exhumed and eroded during the closure of the Slide Mountain Ocean and the subsequent collision with the Laurentian continental margin. We interpret the Manley basin as a syn- to post-collisional extensional basin associated with regional detachment faults that formed because of crustal thickening in the collisional zone. From a regional perspective, an extensive clastic wedge prograded northward away from the zone of crustal thickening and can be identified in a series of Mesozoic sedimentary basins that are discontinuously exposed over 1500 km in southern Alaska. Results of our study better delineate the tectonic processes that set the framework for the construction of the Late Mesozoic and Cenozoic Cordilleran orogen.</p> Sedimentology Structural geology and tectonics Alaska Geology Sedimentology Stratigraphy Tectonics Clastic wedge Paleogeography Intermontane terranes Yukon-Tanana terrane Laurentia Manley basin Paleozoic Devonian Mississippian Mesozoic Cretaceous Accretion tectonics Backarc extension Detrital zircon Slide Mountain Ocean Kahiltna Basin Kuskokwim Basin Wellesley Basin Crustal thickening Fairbanks Schist Wickersham unit Chatanika unit Cascaden Ridge unit Wolverine Quartzite Wilber Creek unit

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Självtranscendens : upplevelse, utveckling och psykologiska förändringar / Selftranscendence : experience, development and psychological changes

DETRITAL RECORD OF PALEOZOIC AND MESOZOIC TECTONICS OF THE NORTHWESTERN CORDILLERAN MARGIN: A CENTRAL ALASKAN PERSPECTIVE