https://theses.otagogeology.org.nz/files/original/ac43a0c6363695e26fc692867aa9acc0.pdf a0c130ae32b5d4cf8cfe4737e79bd7a7 Dublin Core The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/. Title A name given to the resource Geology theses OU Geology thesis Thesis or dissertation completed by University of Otago Geology students Location WKT (WGS84) The location stored in WKT (WGS84) format POLYGON ((170.36594673500008 -45.616639051999982,170.352368813000112 -45.616360025999938,170.208429513000056 -45.613312699999938,170.20884602700005 -45.602641006999932,170.208853985000019 -45.602407127999982,170.210501595000096 -45.560282209999968,170.211186941000051 -45.542747603999942,170.211281533000033 -45.540359609999939,170.249009269000112 -45.541326722999941,170.257128221000016 -45.541532823999944,170.278577376000044 -45.542076501999929,170.400311653000017 -45.545084479999957,170.397636511000087 -45.617282555999964,170.36594673500008 -45.616639051999982)) Author last name Last name of the Author Brown Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? MSc Advisers Who supervised/advised this student Coombs, D.S. Means.W.D. Abstract The Abstract for this thesis The area mapped lies south-east of Middlemarch, Eastern Otago. It is underlain mostly by schist but also includes several small Tertiary outliers of basanitic volcanics resting on a thin formation of quartz sands and conglomerates. The lithology, mineralogy and structure of the schist are reported. From these studies the following conclusions are made: (1) bedding in a wide range of thicknesses is recognizable in the schist, (2) the area lies within a biotite and possibly garnet zone of metamorphism, (3) retrogressive metamorphism occurred and appears to have been accompanied by a deformational phase, (4) there were at least two phases of deformation during the metamorphic period - the first may have produced large-scale recumbent folds. A section on the post-metamorphic geology includes a study of the sedimentary and volcanic formations, post-metamorphic structures, and geomorphology. A post-metamorphic history is given and compared with the regional geology. It appears that the area was stable throughout the lower and middle Tertiary. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Mt Stoker Thesis description Number of pages, maps, CDs, etc. xii., 121 p., Map folded in pocket., photoes and illus., 27cm. Dublin Core The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/. Identifier An unambiguous reference to the resource within a given context 1963Brown Creator An entity primarily responsible for making the resource Brown, Edwin H. Date A point or period of time associated with an event in the lifecycle of the resource 1963 Title A name given to the resource The geology of the Mt. Stoker area Subject The topic of the resource Map Igneous petrology Metamorphic geology Sedimentology Structural geology biotite-?garnet zone retrograde metamorphism