1 10 1 https://theses.otagogeology.org.nz/files/original/6857cd10a2335d979dce10678a8701c8.pdf e1df20bf16ed07d70e66f8da2cfa48fa 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 ((173.518433713491305 -42.414067163873142,173.518220622106099 -42.437002891036855,173.408910896055005 -42.508631583422527,173.366636857463618 -42.507881069880334,173.367349552949293 -42.49209269725079,173.395850516460257 -42.48038159787842,173.39773604199587 -42.46041897251655,173.490311246376649 -42.415978024907737,173.489507324179698 -42.415981460574095,173.518433713491305 -42.414067163873142)) Author last name Last name of the Author Crampton Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Fordyce, R.E. Abstract The Abstract for this thesis The Mesozoic stratigraphy of the Monkey Face area, Marlborough, consists of ?Late Jurassic Torlesse Supergroup rocks overlain unconformably by the terrestrial to shallow marine Arowhanan Stage Bluff Sandstone Member of the Gridiron Formation. Lying with inferred disconformity on this is the shallow marine ?Haumurian Conway Siltstone. Another disconformity marks the base (?Waipawan Stage) of the Amuri Limestone Formation. The top of the Amuri Limestone is not present, and a small block of Altonian siltstone (Waikari Formation) is fault-bounded. The Torlesse Supergroup sandstone is interpreted as having derived largely from recycling of older low-grade Torlesse rocks. Mineralogical and textural maturity of the sediments increases into the Gridiron Formation and Conway Siltstone and indicates continued reworking of this terrane. In addition muscovites in the Conway Siltstone and Waikari Formation document erosion of a schist provenance inferred to be uplifted Torlesse. Folds and faults (reverse, normal, and strike slip) are a consequence of dextural movement on the Hope Fault just to the north of the Monkey Face area. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Monkey Face Thesis description Number of pages, maps, CDs, etc. v. 61 p. ill. Photos. Map (folded in pocket). 30 cm. 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 1985Crampton Creator An entity primarily responsible for making the resource Crampton, JS Date A point or period of time associated with an event in the lifecycle of the resource 1985 Title A name given to the resource The Geology of the Monkey Face area, Marlborough, with special reference to the Mesozoic strata. Subject The topic of the resource Map Sedimentary petrology Paleontology Cenozoic Mesozoic Bluff Sandstone Conway Siltstone Gridiron Formation Torlesse Supergroup