This thesis examines accounts of the life of Ras-chung-pa, also known as rDo- rje Grags-pa (1084-1161), written from the thirteenth to the eighteenth centuries. It identifies what sources are presently available and discusses their inter-relationship. The thesis will present a development of narrative traditions that fuse and eventually climax in the sixteenth century Ras-chung-pa'i rNam-thar by rGod-tshang Ras-pa, which is the standard biography for present-day Tibetan Buddhism. This thesis will reveal how rGod-tshang Ras-pa's version of the first half of Ras-chung- pa's life is a late composite of various conflicting narratives. As the primary source materials have been little studied or even identified, a major part of the thesis will be an exploration and identification of the sources. The thesis will both show how narratives about Ras-chung-pa evolved and suggest their possible historical sources.

Thesis (Ph. D.)--University of Washington. / Bibliography: l. 242-251.

Univ., Magisterarbeit, 2008--Frankfurt (Main). / Engl. Übers. des Hauptsacht.: A medical anthropological study about the doctor-patient relationship.

Diplomarbeit Hochschule für Angewandte Psychologie Zürich, 2005.

A database containing previously published geochronologic, geochemical, and isotopic data on Mesozoic to Quaternary igneous rocks in the Himalayan-Tibetan orogenic system are presented. The database is intended to serve as a repository for new and existing igneous rock data and is publicly accessible through a web-based platform that includes an interactive map and data table interface with search, filtering, and download options. To illustrate the utility of the database, the age, location, and Hf-t composition of magmatism from the central Gangdese batholith in the southern Lhasa terrane are compared. The data identify three high-flux events, which peak at 93, 50, and 15 Ma. They are characterized by inboard arc migration and a temporal and spatial shift to more evolved isotopic compositions. Plain Language Summary A new database with a web-based interface is presented that contains compiled geochronologic, geochemical, and isotopic data on igneous rocks in the Himalaya-Tibetan orogen.

No description available.

With the aim of better understanding the history of ocean closure and suturing between India and Asia, we conducted a geologic investigation of a siliciclastic matrix tectonic melange within the western Yarlung suture zone of southern Tibet (Lopu Range region, similar to 50 km northwest of Saga). The siliciclastic matrix melange includes abundant blocks of ocean plate stratigraphy and sparse blocks of sandstone. Metapelite and metabasite blocks in the melange exhibit lower greenschist fades mineral assemblages, indicating that they were not deeply subducted. We obtained detrital zircon U-Pb geochronologic and sandstone petrographic data from sandstone blocks in the melange and sandstone beds from Tethyan Himalayan strata exposed to the south of the suture. The sandstones from both units are all similar in U-Pb detrital zircon age spectra and petrography to the nearby Tethyan Cretaceous-Paleocene Sangdanlin section, which records the earliest appearance (at similar to 59 Ma) of arc-affinity strata deposited conformably on Indian-affinity strata. Two Paleocene sandstones, one of which is a schistose block incorporated in the siliciclastic matrix melange, yielded indistinguishable maximum depositional ages of similar to 59 Ma. Mesozoic Asian-affinity sandstone blocks previously documented in the siliciclastic matrix melange 200-500 km along strike to the east are notably absent in the Lopu Range region. We documented a gradational transition in structural style from the block-in-matrix melange in the northeast to the south-vergent Tethyan thrust belt in the southwest. Blocks of Tethyan Himalayan strata increase in size and the volumetric proportion of matrix decreases from northeast to southwest. We conclude that no arc-affinity sandstone blocks were incorporated into the subduction complex until India-Asia collision at similar to 59 Ma when the Xigaze forearc basin became overfilled and Tethyan Himalayan strata entered the trench. As collision progressed, there was a gradual transition in structural style from block-in-matrix melange formation to imbricate-style thrust belt formation. (C) 2017 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

No description available.

No description available.

published_or_final_version / Earth Sciences / Doctoral / Doctor of Philosophy