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1. 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 ...


2. Geomagnetic and seismological data collected from Scott Base, Cape Evans (Ross Island) and Lake Vanda [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 ...


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. Examination of the Buckeye Tillite formation, the trace fossils within the Devonian Horlick formation and the Permian Coal Measure in the Ohio Range of the Horlick Mountains [K026_1983_1984_NZ_1]
A second season of field work was undertaken in the Ohio Range of the Horlick Mountains as a three fold geological study to complete the stratigraphy of the area. This included an analysis of the ...


5. 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 ...


6. Geological surveys, seismology, chemistry, geology and lava sampling at the Mt Erebus summit crater to investigate the behaviour of the volcano [K044_1972_1982_NZ_1]
An international study of the volcanic activity and geological processes taking place on Mt Erebus were investigated over 10 seasons. The broad program involved several investigations. ...


7. 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 ...


8. 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. ...


9. Field mapping data and petrological collections for petrography, geochronology and geochemistry, of rocks from Mt Morning, southern Victoria Land, Antarctica [K062_2004_2006_NZ_1]
Mt Morning is the most southerly of a series of central type volcanoes that make up the McMurdo Volcanic Group of south Victoria Land. It is characterised by a trachyte - basanite - phonolite assemblage. ...


10. 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 ...


11. 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 ...


12. Early geological, glaciology and biological investigations of the McMurdo Dry Valleys, the Koettlitz Glacier area and Darwin Glacier area by Victoria University of Wellington Antarctic Expeditions [K042_1957_1963_NZ_1]
The Victoria University of Wellington Antarctic Expedition (VUWAE) was mounted to complete the detailed investigations of the extensive ice free area of Victoria Land between the Taylor and Mackay ...


13. Field and petrographic descriptions of the outcrops of the McMurdo Volcanic Group in the Royal Society Ranges, northwest of the Koettlitz Glacier [K002_1977_1978_NZ_2]
Detailed field and petrographic observations of the outcrops of McMurdo Volcanics Group in the Southern Foothills of the Royal Society Range from Foster Crater in the south to Marshall Valley in the ...


14. Marine Seismic Surveying in McMurdo Sound [K042_1979_1980_NZ_4]
A marine seismic survey was conducted in McMurdo Sound to extend marine seismic coverage to i) the western side of McMurdo Sound, in order to examine the nature of any faulting or other structures ...


15. 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 ...


16. 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 ...


17. Determination of a polar wander path for Beacon Supergroup at Mount Bastion, West Beacon and Table Mountain [K042_1978_1979_NZ_1]
The Beacon Supergroup in the McMurdo Sound region is a flat lying continental sequence about 2000m thick and ranging in age from Early Devonian to Late Triassic (400 to 180 my BP). A polar wander ...


18. Determination of deposition, sediment transport direction and age of New Mountain Sandstone (Beacon Supergroup) at various localities in the Royal Society Range and Dry Valleys region [K042_1974_1975_NZ_4]
The New Mountain Sandstone, the lowest formation of the Beacon Supergroup was studied in detail at various localities in the Royal Society Range and Dry Valley's region to determine its environment ...


19. Geological examination and sampling of Devonian Aztec Siltstone, the fish bearing red bed sequence and Permian coal measures for pollen and coal rank studies [K042_1973_1974_NZ_1]
Sections of Aztec siltstone at Mt Metschel, in the Alligator Peak area, Shapeless Mountain, Mount Fleming, the Lashly Mountains and Aztec Mountain were examined and sampled on a very detailed scale ...


20. Geological examination, mapping and sampling of the Mawson Volcano breccias at Shapeless Mountain and Allan Hills [K042_1972_1973_NZ_2]
A detailed study and sampling programme of the Mawson volcano breccia was carried out at Shapeless Mountain and on neighbouring Mistake Peak. Paleomagnetic measurements were used to determine the ...


21. Geological examination, stratigraphic sections, mapping and sample collection of Beacon and Ferrar rocks and fossils in the area between the Skelton Neve and the Mackay Glacier [K042_1971_1972_NZ_3]
Beacon and Ferrar rocks were studied just west of the Dry Valleys, between the Skelton Neve and the Mackay Glacier area. Detailed stratigraphic sections were measured with staff and level at Mistake ...


22. Geological investigation and mapping of the Wellar Coal Measures to determine the depositional environment [K042_1979_1980_NZ_1]
In the 1978-79 field season, the Beacon Supergroup and the intruding Ferrar Dolerite were mapped at Mt Fleming and Horseshoe Mountain including three laterally related sections of the Wellar Coal ...


23. Geological investigations in the Fry Glacier region [K042_1976_1977_NZ_4]
Geological reconnaissance was conducted in the Fry Glacier region to study in some detail the glacial geology of the Dry Valley areas and exposures of the Beacon Supergroup there. Geological mapping ...


24. Geological investigations of the Cambrian and Beacon sediments in the Bryd Glacier/Darwin Glacier region [K042_1978_1979_NZ_2]
Cambrian and Beacon sediments in the Byrd Glacier region of the Darwin Mountains were investigated. The sites visited included Mt Rainbow, Kiwi Pass, Mt Egerton, Mt Durnford, Mt Field, Mt Tuatara, ...


25. Geological investigations of the basement rocks in the Evans Neve area, North Victoria Land [K042_1971_1972_NZ_2]
The basement rocks in a small area on the eastern edge of the Evans Neve, north Victoria Land were studied. The areas visited and examined included Mt Overlord, Mt Goby and the Retreat Hills, The ...


26. Geological mapping and examination of the Beacon SuperGroup in Victoria Land: Beacon Heights, Skelton Neve, Portal Mountain and Horseshoe Mountains, Allan Hills, Darwin Mountains and Victoria Valley area [K042_1970_1971_NZ_1]
The stratigraphy of the Beacon Super Group in the Beacon Heights was previously described. This study was continued this season, extending the stratigraphy northward to the Mackay Glacier and southward ...


27. Geological mapping and investigations of the Permian Maya Erosion Surface, Metschel Tillite, Pre-Pleistocene tills and Wellar Coal Measures in the Upper Taylor Glacier area and Coombs Hills [K042_1977_1978_NZ_2]
Geological investigation in the upper Taylor Glacier was conducted and had three objectives; 1) To locate and examine at Kennar Valley, Finger Mountain and Mount Feather, within the Quartermain Mountains ...


28. 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 ...


29. 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 ...


30. Geochemistry, petrology and structure of Mt Dromedary/Koettlitz glacier area [K002_1970_1974_NZ_1]
Geological investigations and mapping was conducted in the Mt Dromedary/Koettlitz Glacier area over two field seasons. Detailed geological mapping was conducted at a 1:50,000 scale. Sufficient samples ...


31. Geological investigations of geological markers and UTh-He apatite analysis of collected samples to determine the nature, amount and timing of vertical and horizontal deformation along the Transantarctic Mountains [K101_2002_2003_NZ_1]
Geological investigations were conducted to better constrain the nature, amount and timing of vertical and horizontal deformation along the Transantarctic Mountains. Geological markers, both horizontal ...


32. Geological investigations of the Robertson Bay Group in the Cape Hallett/Cape Christie area [K003_1967_1968_NZ_1]
Geological investigations were conducted in the Cape Hallett/Cape Christie area to examine rocks and structures of the Robertson Bay Group and to make comparisons with New Zealand rocks, South East ...


33. Geological investigations of the fault lines in the rocks of the Transantarctic Mountains in the area of the Wilson Piedmont Glacier to understand uplift of the mountain range [K112_1997_1998_NZ_1]
Inferred fault lines in the rocks of the Transantarctic Mountains in the area of the Wilson Piedmont Glacier were investigated to add to the understanding of the uplift of the mountain range. Specifically, ...


34. Geological mapping (1:25,000) of the western parts of the Asgard and Olympus Ranges, South Victoria Land [K112_1982_1983_NZ_2]
Geological mapping at a scale of 1:25,000 of the western parts of the Asgard and Olympus Ranges adjacent to Mt Fleming and Shapeless Mountain was completed. A total area of 950 km2 was mapped. Three ...


35. Geological mapping 1:50,000 in the Convoy Range and determining the glacial history through surficial deposit mapping and investigations [K112_1989_1990_NZ_1]
1:50,000 geological mapping of the Convoy Range was conducted covering an area of some 2,500 square kilometres extending from the Mackay Glacier in the south to the Fry and Chattahoochee Glaciers ...


36. Geological mapping 1:50,000 in the Thundergut area (Olympus and Asgard Range, Taylor Glacier), South Victoria Land [K112_1988_1989_NZ_1]
1:50,000 geological mapping of the Thundergut area was conducted covering an area from the western tip of the Kukri Hills, as far west as the Solitary Rocks, Friis Hills and Asgard Ranges and as far ...


37. Geological mapping 1:50,000 in the areas between the Asgaard and Clare Ranges, South Victoria Land [K112_1992_1993_NZ_1]
Geological mapping 1:50,000 was conducted in South Victoria Land to draw together previous mapping works to produce a map of the geology between the Asgaard and Clare Ranges. Previous work includes ...


38. Geological mapping 1:50,000 in the upper Ferrar Glacier area: the massifs of Pivot Peak, Terra Cotta, Knobhead, Table Mountain and Rotunda [K112_1987_1988_NZ_1]
1:50,000 geological mapping was conducted at the head of the Ferrar Glacier including the massifs of Pivot Peak, Terra Cotta, Knobhead, Table Mountain and Rotunda. The exposed rocks are almost entirely ...


39. Geological mapping of the Beacon Supergroup at Mt Bastion, Skew Peak and Robinson Peak, South Victoria Land [K112_1984_1985_NZ_1]
The coal measure sequence in the Beacon Supergroup extends northwards from the Upper Wright Valley towards the Willett Range area (Mt Bastion/Skew Peak/Robison Peak). An area approximately 1,000km2 ...


40. Measurement of the earth's total magnetic field ahd seismic profile measurements between New Zealand and McMurdo Sound [K004_1963_1964_NZ_1]
Measurements of the earth's total magnetic field was conducted on board the HMNZS Endeavour from New Zealand to McMurdo Sound. Measurements were made with a proton magnetometer designed and trialled ...


41. 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 ...


42. 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? ...


43. Geological mapping and reconnaissance of the Edward VII Peninsula, Marie Byrd Land [K151_1987_1988_NZ_1]
A field expedition visited all of the rock outcrops in the Edward VII Peninsula, Marie Byrd Land. The principal objective was to undertake geological studies and make collections for future geochronological ...


44. Geological mapping in the Lake Victoria and Lake Vida areas to allow basement rock types in this area to be correlated with the described intrusive sequence [K403_1988_1989_NZ_1]
The Dry Valley Drilling Project hole 6 from the western end of Lake Vida intersected Olympus Granite Gneiss and Vida Granite. Previous work on this area included uranium-lead dating analysis on core ...


45. 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 ...


46. 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 ...


47. Geological and laboratory analysis of rock samples from the Ruppert Coast-Hobb Coast, Marie Byrd Land, Kohler Range and Bear Peninsula to understand the Mesozoic Pacific ocean during Gondwanaland breakup [K051_1990_1993_NZ_1]
Prior to the breakup of Gondwanaland there was an entire southern rim to the Pacific extending from New Calendonia through New Zealand, West Antarctica to Patagonia. Understanding the Mesozoic tectonics ...


48. Geological investigation (mapping, geochronology and geochemical analysis) of West Antarctica Volcanics from Marie Byrd Land [K048_1989_1991_NZ_1]
The West Antarctica Volcano Exploration (WAVE) project was conducted to gain an understanding of the volcanic and geochemical evolution of intraplate volcanoes in West Antarctica and to compare volcanism ...


49. Geological investigation of the stratigraphic succession through the thickest portion of the Bowers Groups and rock and fossil samples for paleontological and depositional dating, Bowers Mountains, Northern Victoria Land [K051_1973_1974_NZ_1]
The Lower Paleozoic rocks of North Victoria Land occupy a key position in any reconstruction of the New Zealand/Australian/Antarctic segment of Gondwanaland. To know the precise age of the Antarctic ...


50. Geological mapping and observations of the regional extent of the Bowers Supergroup and the rock sequences flanking it: Wilson Group and Robertson Bay Group, North Victoria Land [K051_1981_1982_NZ_1]
The stratigraphy, structure, paleontology and sedimentology of the Lower Paleozoic Bowers Supergroup is fairly well known but some questions remain unanswered. The objective of the expedition was ...


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