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1. Biostratigraphic collections of Devonian fish fossils from Middle Devonian Aztec Siltstone at the top of the Taylor Group (Beacon Supergroup) and sediment studies for a basin analysis [K026_1991_1992_NZ_1]
Using toboggans and sledges, the party travelled 700 kilometres from the Darwin Glacier northwards to the Lashly Mountains to study Taylor Group sedimentary rocks (Beacon Supergroup). The principle ...


2. Provenance analysis of Cambrian conglomerates, Northern Victoria Land [K051_2000_2003_NZ_1]
The Cambrian volcanic arc of North Victoria Land and the Cambrian arc of NW Nelson (NZ) are strikingly similar. They are of island arc character but both now lie within continental crust. In NVL ...


3. Geomagnetic and seismological data collected from Scott Base, Cape Evans (Ross Island) and Lake Vanda [K102_1959_2008_NZ_1]
Geomagnetic and seismological measurements were established in Antarctica in 1957 as part of the International Geophysical Year and have continued until present. Geomagnetic data have been recorded ...


4. Geomagnetic and seismological data collected from Scott Base, Cape Evans (Ross Island) and Lake Vanda - K102_1959_2012_NZ_1 [K102_1959_2012_NZ_1]
Geomagnetic and seismological measurements were established in Antarctica in 1957 as part of the International Geophysical Year and have continued until present. Geomagnetic data have been recorded ...


5. Oceanography, sea seismic surveys and benthic surveys of the New Zealand sub-Antarctic Islands areas (Auckland and Campbell Islands), the Macquarie Ridge area and the ocean between New Zealand and the Ross Sea [K002_1959_1963_NZ_1]
Oceanographic, sea seismic surveys and benthic surveys were conducted aboard research vessels (HMNZS Endeavour, Wilhoite, Rotoiti, USS Burton Island) between 1959 and 1963. The principal aim of the ...


6. Palaeozoic Terrane Correlation: New Zealand and Antarctica [K051_2003_2004_NZ_2]
In St Johns Range and eastern Olympus Range, unusually coarse lithologies at the base of the Beacon Supergroup have the potential to provide significant information on the provenance of the earliest ...


7. Paleomagnetic samples and geological mapping of the basement geology of the Daniels Range and the Rennick Glacier area in North Victoria Land [K017_1981_1982_NZ_1]
A collection of paleomagnetic rock samples including Jurassic volcanics and dolerites, Beacon Supergroup, Devonian-Carboniferous volcanics, Paleozoic Granitoids and Cambrian Volcanics and sediments ...


8. Paleozoic tectonics of the Gondwana margin: Provenance of the Sperm Bluff Conglomerate. Implications for Cambrian tectonics and Devonian and younger paleotectonics and paleogeography [K051_2003_2004_NZ_1]
The basement rocks of eastern Northern Victoria Land (NVL) consist of a series of exotic terrances that were accreted to the Gondwanan margin while Andean style convergence was occurring. Conversely, ...


9. Regional stratigraphy, sedimentology structure, metamorphic and tectonic history of the lower grade Skelton Group meta-sediments between the Skelton and Koettlitz Glaciers [K002_1975_1976_NZ_1]
A study of the low grade meta-sedimentary rocks of the Skelton and Koettlitz Glacier areas including the unmapped Mt Cocks Range at the head of the Koettlitz Glacier was investigated to add to the ...


10. Sedimentological and palaentological examination of the Devonian Horlick formation in the Ohio Range of the Horlick Mountains [K026_1979_1980_NZ_1]
15 sections of the Horlick formation were measured in detail along the Ohio escarpment from Discovery Ridge to Lackey Ridge. The Ohio Range contains the only well exposed record of unequivocally marine ...


11. Sedimentological and structural measurements and rock samples for radiometric dating of the Swanson Group and Ford Granodiorite of the Ford Ranges, Marie Byrd Land, West Antarctica [K051_1978_1979_NZ_1]
The purpose of the expedition was to examine in detail the pre-Cenozoic geology of the Ford Ranges which comprise the main area of exposed rock in western Marie Byrd Land and the type area of two ...


12. Seismic profile survey of McMurdo Sound and Terra Nova Bay [K042_1974_1975_NZ_2]
As part of the Dry Valleys Drilling Project, the area of the McMurdo Sound drill hole was surveyed with a seismic survey profile and extended to cover the whole of the McMurdo Sound region to determine ...


13. Seismic refraction surveys in the McMurdo Sound region [K042_1964_1965_NZ_5]
The suitability of first arrival seismic refraction apparatus for surface structure studies was investigated at sites in the Wright, Taylor and Miers Vallyes and on Brown Peninsula. Results show that ...


14. Seismic, infrasonic and magnetic induction data from Mt Erebus: 1980-1986, The International Mt Erebus Seismci Survey (IMESS) [K044_1980_1986_NZ_1]
The International Mt Erebus Seismic Survey (IMESS) was conducted on Mt Erebus to monitor and assess the seismic activity of the volcano year round. Seismic, infrasonic and magnetic induction data ...


15. Seismograph data from the David Glacier region near Terra Nova Bay to determine the origins of low magnitude seismicity in the area: brittle ice failure, basal shearing beneath the glacier, or tectonic events? [K101_2003_2004_NZ_1]
Temporary seismograph stations placed in the Transantarctic Mountains have recorded regular, low magnitude seismicity. The origin of the quakes could not be uniquely discriminated among brittle ice ...


16. Soil, relic ice, permafrost, Hart Ash and granite samples from the Lower Victoria Valley, Beacon Valley, near the Meserve Glacier in Wright Valley, and Kennar Valley to determine the deposition of this ice [K047_2004_2006_NZ_1]
Ancient glacial ice that has stagnated and lies buried underneath rock debris has been found in the Beacon Valley and more recently in several other valleys. This ice poses the possibility of obtaining ...


17. Statigraphy of the Heimdall and Conrow Glacier area [K026_1976_1977_NZ_2]
The stratigraphy of the Heimdall and Conrow Glacier area was determined to compliment earlier work carried out by Victoria University Antarctic Expeditions to define the stratigraphy of the area between ...


18. Structural geology, sedimentology and geological mapping of the Robertson Bay Group along a traverse from the Pitkevitch Glacier to the Millen Range, North Victoria Land [K002_1981_1982_NZ_1]
A traverse from the head of Pitkevitch Glacier to the Millen Range was undertaken to investigate details of the structural geology and sedimentology of the Robertson Bay Group and its correlation ...


19. Teleseismic and local earthquake measurements with an digital seismometer array spread between the McKay Glacier and Table Mountain (to the north and south) and Cape Bird and Mt Fleming (to the east and west) [K102_1999_2000_NZ_1]
A digital seismometer array (10 station) was placed in the Transantarctic Mountains over a three month period (November 1999-January 2000) to record teleseismic (distant earthquakes more than 20° ...


20. The Devonian trace fossils of the Taylor Group in the Darwin Glacier area [K026_1988_1989_NZ_1]
The principle aim of this expedition was to extend the knowledge of Devonian trace fossils in the Taylor Group in the Darwin Glacier area, to relate them to earlier published research in the Dry Valley ...


21. The Heimdall Erosion surface [K051_2006_2007_NZ_1]
The Heimdall Erosion surface between Mt Jason, Mt Hercules, Mt Electra, Balham Valley, Vashka Lake and Sponsors Peak was investigated with the aim to evaluate the tectonic setting of early Beacon ...


22. The Heimdall and Kukri Erosion surfaces [K051_2007_2008_NZ_1]
The Heimdall Erosion Surface was followed southwards from the Olympus Range through the Asgard Range and onward to the mountains south of the Taylor-Ferrar Glaciers where it is said to die out or ...


23. The direction of magma flow and behaviour of the magma in the formation of the Ferrar Large Igneous Province 180 million years ago, Pandora Spyre and Terra Cotta Mountain, Victoria Land [K061_2007_2008_NZ_1]
Exposed at Terra Cotta Mountain and Pandora Spyre are vertical bladelike bodies of basaltic rock which cut across older pale colored sedimentary rocks. The pathway the magma took to the earth's surface ...


24. The direction of magma flow in the formation of the Ferrar Large Igneous Province 180 million years ago, Coombs Hills, Victoria Land [K061_2005_2006_NZ_1]
Exposed at Coombs Hills are vertical bladelike bodies of basaltic rock that cut across older white sedimentary rocks and through deposits of a Jurassic volcanic complex (Mawson Formation). The majority ...


25. The direction of magma flow in the formation of the Ferrar Large Igneous Province 180 million years ago, Mt Gran and Terra Cotta Mountain, Victoria Land [K061_2004_2005_NZ_1]
An outcrop of the 'plumbing system' of one of the largest volcanic events known was investigated at Mt Gran and Terra Cotta Mountain (Victoria Land) to determine how magma reached the surface to feed ...


26. The distribution of intrusive plutonic igneous rocks at Reeves Bluff and the Western Worcester Ranges by geological mapping and geochemical and geochronological analysis of samples [K062_2001_2002_NZ_1]
The relationship between the processes of metamorphism, magmatism and deformation that took place during the Ross Orogeny has been investigated. Previous work has established that the relationship ...


27. The geology of the Nimrod Glacier - Beaumont Bay area [K002_1960_1961_NZ_2]
The geology of the Nimrod Glacier - Beaumont Bay area was examined to describe the structure, formation and depositional history of the region. Three types of sedimentary rock types were present in ...


28. The geology of the ridges between the Campbell and Aviator Glaciers and Franklin Island, north Victoria Land [K002_1966_1967_NZ_3]
The geology of the ridges between the Campbell and Aviator Glacier, north Victoria Land, was investigated. The oldest rocks in the area are early Paleozoic or PreCambrian metasediments and metavolcanics ...


29. The geothermal and volcanic activity of Mt Melbourne and Mt Erebus [K044_1972_1973_NZ_1]
The geology and the geothermal and volcanic activity of Mt Melbourne and Mt Erebus was investigated by surveying the summit craters of each volcano. At Mt Melbourne, the thermal activity was investigated ...


30. The physical features and dynamics of Ferrar dolerite dykes and sills within the Allan Hills, Victoria Land [K061_2006_2007_NZ_1]
At Allan Hills, dykes and sills are respectively sub-vertical and sub-horizontal magma bodies of fine textured basaltic rock, remnants of the formation of the Ferrar Large Igneous Province when large ...


31. The pre-Devonian structural and metamorphic history of the basement in the Victoria and Wright Valleys [K042_1984_1985_NZ_1]
The pre-Devonian structural and metamorphic history of the basement in the Victoria and Wright Valleys, with emphasis on the depth of burial and amount of uplift prior to Beacon sedimentation, was ...


32. The relationship between major rock groups in the region around the Rennick Glacier, North Victoria Land [K002_1967_1968_NZ_1]
The relationship between major rock groups in the region around the Rennick Glacier was investigated including the Robertson Bay Group (greywacke and argillites), the Bowers Group (shallow water sediments, ...


33. The stratigraphy and magnetostratigraphy of surface and subsurface late Cenozoic Ross Sea drift from drill cores taken in the eastern Taylor Valley [K010_1980_1983_NZ_1]
In the 1980/81 and 1982/83 Antarctic field seasons, drilling and mapping were undertaken as part of a programme in the eastern Taylor Valley to investigate the late Cenozoic glacial history of the ...


34. Topographical and geological mapping and investigations of the areas around the Holyoake, Cobham, Swithinbank and Queen Elizabeth Ranges [K002_1964_1965_NZ_1]
Previous mapping of the Miller Range (1961-1962) and the Holyoake Range (60-61) resulted in a generalized stratigraphy for the region but comparisons were tentative as the rock sequences were completely ...


35. Topographical and geological surveys and biology and soil sampling of the Queen Maud Mountains bordering the Ross Ice Shelf between the Axel Heiberg and Shackleton Glaciers [K002_1963_1964_NZ_2]
Geological and topographical surveys were carried out in the mountains bordering the Ross Ice Shelf between the Axel Heiberg and Shackleton Glaciers. The objective was to establish what major rock ...


36. Topographical and geological surveys and biology and soil sampling of the area between the Mawson and Preistly Glaciers, North Victoria Land [K002_1962_1963_NZ_1]
Survey work sufficient to provide ground control for topographical mapping was carried out. The area mapped included the part of North Victoria Land bounded by the Mawson Glacier in the south and ...


37. Topographical and geological surveys and biology and soil sampling of the area between the Pennell and Tucker Glaciers to the Oates Land coast in north Victoria Land [K002_1963_1964_NZ_1]
An area roughly bounded by the Matusevich Glacier (157°, 30'E) in the west to the Tucker Glacier in the east and from 72° S north to the Oates Land coast was examined in reconnaissance fashion, including ...


38. Topographical and geological surveys at Carapace Nunatak, Allan Nunatak and the Coombs Hills, Victoria Land, Antarctica [K002_1964_1965_NZ_2]
A detailed geological study of Carapace Nunatak, Allan Nunatak and the Coombs Hills at the head of the Mawson and Mackay Glaciers was conducted. The whole are was systematically covered with three ...


39. Topographical and geological surveys of the area at the head of the Priestly, Campbell, Aviator, Mariner and Rennick Glaciers, North Victoria Land [K002_1962_1963_NZ_2]
The area at the head of the Priestly, Campbell, Aviator, Mariner and Rennick Glaciers and eastwards to the coast was surveyed by a basic triangulation network and ground photography, some 14,000 square ...


40. Video surveillance recordings and seismic activity of Mt Erebus: 1986-1991, The International Mt Erebus Eruption Mechanism Study (IMEEMS) [K044_1986_1991_NZ_1]
Studies of the location of earthquake foci at Mt Erebus found that eruption earthquakes had an apparent range of depths to 4km, but that infrasonic signals were more consistant with a surface origin. ...


41. Volcanic and geothermal activity of Mt Melbourne [K002_1966_1967_NZ_2]
The southern side of Mt Melbourne was ascended to examine the present day thermal activity and the evidence for historic volcanism of the mountain. Many small recent looking volcanic cones and mounds ...


42. Volcanogenic and sedimentary deposits at Mt Watters [K042_2000_2001_NZ_1]
Volcanogenic and sedimentary deposits that comprise Mt Watters were mapped and sampled at Allan Hills to determine the nature of the feature and the eruptive event which produced it. Collected data ...


43. Volcanology and sedimentology of the phreatomagmatic eruptive system of the Mawson Formation in Coombs Hills, Victoria Land, Antarctica [K061_1999_2000_NZ_1]
The volcanology and sedimentology of a phreatomagmatic eruptive system in the Coombs Hills, Victoria Land was investigated to determine how magmatism is initiated and evolves during continental rifting. ...


44. 1:25,000 geological mapping of the St Johns Range from the central Wright Valley to the Mackay Glacier and from the Miller Glacier to west of Victoria Valley [K112_1990_1991_NZ_1]
The DSIRGEO mapping programme in the 1990/91 season was designed to link the area covered in 1989/90 (Convoy Range) with that covered in 1988/89 (Thundergut Sheet). The eventual aim of the programme ...


45. A reconstruction of the record of volcanic processes within the vent of a large and explosive basaltic eruption in the Mawson Formation in the Allan Hills [K061_2001_2002_NZ_2]
The contact relationship between volcanic deposits and surrounding country rocks of the Beacon Supergroup are steep over a large area. Beyond the landslide deposits along the contact between Beacon ...


46. A seismic refraction survey on sea ice near Butter Point, New Harbour, McMurdo Sound [K042_1980_1981_NZ_1]
A seismic refraction survey was conducted on sea ice near Butter Point to provide data on sediment thickness for possible further drilling and to investigate the cause of a reported gravity anomaly. ...


47. Age determination of the detrital zircon component of crustal slices of Ross Orogen from the Skelton Glacier and Royal Society Ranges areas [K062_2003_2004_NZ_1]
It is suggested that the Ross Orogeny is composed of a wide variety of crustal slices that are exotic to their present location and were accreted to the East Antarctic craton during the lower paleozoic ...


48. An integrated marine geophysical survey (multibeam bathymetry, chirp sonar, gravity and geomagnetic measurements, with seismic reflection) of the southern Adare Basin region. (R/V Nathaniel B Palmer cruise NBP0701) [K101_2006_2007_NZ_1]
A detailed integrated marine geophysical survey of the sourthern Adare Basin region and a series of detailed seismic transects across the Northern Basin, underlying the north-western Ross Sea continental ...


49. Broadband seismic wavefield data recorded at a temporary array in the Transantarctic Mountains (TAM) [TAM-bband-9900]
These earthquake data contain broadband seismic wavefield recordings, as recorded by a temporary array placed in the Trans-antarctic Mountains during the summer of 1999-2000. The experiment was carried ...


50. Collaborative Research: Geochemical transect from oceanic Adare Basin to adjacent continental Adare Peninsula: implications for the origin of intraplate (HIMU-like) alkaline magmas [SIO_BGSU_ADARE_GEOCHEM]
Detailed analytical studies are still being conducted on Adare Basin samples, but preliminary results for their major element, trace element and Sr-Nd-Pb isotopic compositions resemble those of volcanic ...


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