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51. GPR profiles and sediment samples from raised beaches along the McMurdo Sound coast to understand the composition, make up and mode of contruction of the beaches [K015_1998_2000_NZ_1]
Due to the continued uplift of the coastline as a response to the retreat of the last glacial maximum ice sheet, beaches are raised above the level of wave and ice push activity and are essentially ...


52. GPR surveys and sand samples for OSL dating and studies of grainsize, petrology and sediment provenance of Victoria Valley sand dunes [K015_2006_2007_NZ_1]
The structure and evolution of sand dunes in Victoria Valley was investigated by completing a GPR survey (with 50, 100, 200, 250, 400, 450 and 900 MHz antennae) to successfully image dune structure ...


53. GPR surveys and sediment sampling for OSL dating to determine the formation of fossil marine deltas in the vicinity of Wales and Commonwealth streams, New Harbour [K015_2004_2005_NZ_1]
The subsurface sedimentary structures that make up New Harbour deltas were investigated using GPR to develop a model for the formation of the fossil marine deltas that are well preserved along the ...


54. Geochemical and geomorphological investigations of the McMurdo Dry Valleys freshwater and saline water bodies [K211_1963_1987_NZ_1]   CHILD DIFs
Since the 1963-1964 season, Japanese scientists have studied major and trace elements, nutrient matter, stable and radioactive isotopes and organic constituents in lakes and ponds and geological samples ...


55. Geochemical studies on the rocks in the McMurdo Sound region [K042_1977_1978_NZ_1]
Geochemical studies were conducted in the McMurdo Sound region. Mossbauer spectrocopic studies of Desert Varnish, the physical and chemical weathering processes of the lavas on Ross Island and bedrock ...


56. Geochemical studies, the natural abundance of nitrogen isotopes in soil and evaporates and observations of the sequential changes in the saline lakes of the Dry Valleys and surrounding areas [K211_1978_1979_NZ_1]   PARENT DIF
Geochemical studies on the tritium chronology of Lake Vanda, the natural abundance of nitrogen isotopes in soil and evaporites in the Dry Valleys and observations of the sequential changes in the ...


57. Geochemistry investigations of landforms in the Ross Sea Region to determine past glacial history and landform processes [K009_1969_1970_NZ_1]   PARENT DIF
The geochemistry of Ross Island (Cape Barne and Cape Crozier), the Taylor and Wright Valleys, Lake Vida in Victoria Valley and Marble Point was studied (weathering and land formation) to determine ...


58. Geochemistry, paleomagnetism and intrusive history of the Ferrar Dolerites, Antarctica [K061_2004_2007_NZ_1]
A suite of geological samples were collected in the Transanatarctic Mountains for paleomagnetic and geochemical analysis. Combined with field observations, these samples will help determine magma ...


59. 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 ...


60. Geodetic (data) survey marks for a geodetic referencing system in the Ross Sea Region: Scott Base GPS continuous tracking station [K150_2004_2008_NZ_1]
A number of survey stations are in use in the Ross Sea Region by both the USAP and NZAP. All of the survey stations have been visited to connect and unify all current survey datums in use in the area ...


61. Geological and geomorphic data and Sirius Group core analysis (stratigraphy, petrographical analysis, ground temperature and isotope analysis) from Table Mountain to determine the depositional history [K047_1996_1997_NZ_1]
The depositional and post depositional history of the Sirius Group tillite in the Dry Valleys area was investigated to resolve the ongoing debate as to whether the East Antarctic ice sheet formed ...


62. Geological and geophysical investigations of the crustal structure and geological processes of the Victoria Land basin and the Iselin Bank areas [K101_1983_1984_NZ_1]
The geological structure and processes of parts of the Ross Sea continental shelf and margin was investigated via the USGS research ship S.P.LEE. The geological structure was investigated from the ...


63. 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 ...


64. 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 ...


65. 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 ...


66. 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 ...


67. 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 ...


68. 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 ...


69. Geological investigation into the mode of origin of the Wright and Taylor Valleys [K042_1969_1970_NZ_2]
The Labyrinth area in the Wright Valley is an unusual area of very steep gullies with flat treads between, which form a box canyon type topography. The mode of origin of the area is a controversial ...


70. Geological investigation of the Priestly Formation and Snowy Point Gneiss Complex in the Berg Mountains from Terra Nova Bay to Campbell Glacier, Oates Coast, North Victoria Land: GANOVEX VII [K002_1992_1993_NZ_1]
As part of the GANOVEX VII Expedition (German Antarctic North Victoria Land Expedition) two research topics were investigated; a) the passage of metasedimentary Priestley Formation into gneisses of ...


71. Geological investigation of the depositional setting of Beacon rocks in south Victoria Land including the Darwin Mountains, Cook Mountains, Britannia Range and the Convoy Range in Allan Hills [K042_1988_1989_NZ_2]
Devonian strata from south Victoria Land has been variously interpreted as marine and non-marine due to the presence of trace fossils that have previously been considered to indicate marine environments ...


72. 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 ...


73. Geological investigations (locations, descriptions, chemical and petrographic analysis) of the coal seams in the Upper Wright Valley [K112_1982_1983_NZ_1]
The presence of coal seams in the Permian strata and to a lesser extent in the Mesozoic sequences in the vicinity of the Upper Wright Valley, South Victoria Land were investigated. Detailed geological ...


74. Geological investigations and collection of fossil specimens from the Sledgers Glacier-Mariner Glacier region to determine the geological history and environment of deposition of the region [K003_1974_1982_NZ_1]
The eastern part of the Bower Group in the Mariner Glacier area and the central western part of the Bowers Group in the Black Glacier-Sledger Glacier area were visited and examined to search for fossils ...


75. Geological investigations and mapping of the Campbell-Priestley Glaciers divide [K002_1965_1966_NZ_1]
The volcanic outcroppings at the head of the Aviator Glacier and the outcrops of the Campbell-Priestley Glaciers divide were investigated and geologically mapped to connect work completed in the 1961-62 ...


76. Geological investigations and topographical surveying of the head of the Beardmore Glacier area [K002_1965_1966_NZ_2]
The stratigraphy of the Buckley Coal Measures and Shackleton Limestone outcrops was investigated and a theodolite surveys of the head of the Beardmore Glacier area was completed. The area mapped consists ...


77. 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 ...


78. 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 ...


79. 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, ...


80. Geological investigations of the Preistly and Campbell Glacier region, Terra Nova Bay [K002_1969_1970_NZ_1]
In the 1962-63 season, a rapid reconnaissance of the geology of the Terra Nova Bay region was conducted. Approximately 100 rock samples were collected and analysed by thin section analysis. In the ...


81. 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 ...


82. 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 ...


83. 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, ...


84. Geological investigations, triangulation surveys and glaciology investigations of the Upper Tucker Glacier area, North Victoria Land, and around Scott Base [K002_1962_1963_NZ_3]
Intensive geological work was conducted in the Tucker Glacier area of North Victoria Land. The work area overlapped the Geological Survey of the 1957-58 Expedition and this was helpful to correlate ...


85. 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 ...


86. 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 ...


87. 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 ...


88. 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 ...


89. 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 ...


90. Geological mapping and analysis of granitoid basement rocks near the Carlyon Glacier and Brown Hills area to determine the tectonic environment during the Ross Orogeny [K062_2000_2001_NZ_1]
The Ross Orogeny refers to a sequence of geological events when East and West Antarctica met, resulting in subduction with associated deformation, crustal thickening, metamorphism and igneous activity. ...


91. 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 ...


92. Geological mapping and examination of the Feather Conglomerate and the Lashly Formation at Horseshoe Mountain and Shapeless Mountain [K042_1979_1980_NZ_2]
Five days were spent geological mapping and sampling at Horseshoe Mountain. The strata cropping out are the Feather Conglomerate (Late Permian - early Triassic) and the Lashly Formation (Mid-Late ...


93. Geological mapping and geochemical and geochronological analysis of anomalous plutonic rocks in the Koettlitz Walcott Glacier and Skelton-Glacier and Hoopers Crags area [K062_1997_1999_NZ_1]
The Ross Orogeny refers to the collision event when East and West Antarctica met, resulting in subduction with associated deformation, crustal thickening, metamorphism and igneous activity. In the ...


94. Geological mapping and geochemical and geochronological analysis of metamorphic basement rocks and the McMurdo volcanics in the Skelton-Glacier and Hoopers Crags area [K062_1998_1999_NZ_1]
The Ross Orogeny refers to the collision event when East and West Antarctica met, resulting in subduction with associated deformation, crustal thickening, metamorphism and igneous activity. The nature ...


95. Geological mapping and geochemical and geochronology analysis of rock samples from Panarama Ridge in the Koetllitz-Walcott Glacier area [K062_1997_1998_NZ_1]
The Ross Orogeny refers to the collision event when East and West Antarctica met, resulting in subduction with associated deformation, crustal thickening, metamorphism and igneous activity. In the ...


96. 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 ...


97. Geological mapping and investigations of the geology of the east and north of North Victoria Land: GANOVEX I Expedition [K002_1979_1980_NZ_2]
The first GANOVEX Expedition (German Antarctic North Victoria Land Expedition) was carried out aboard the M.V. Schepelsturm, a large ocean going anchor and cable handling tug. Field activities were ...


98. Geological mapping and investigations of the geology of the east and north of North Victoria Land: GANOVEX III Expedition [K002_1982_1983_NZ_2]
The third GANOVEX Expedition (German Antarctic North Victoria Land Expedition) was carried out aboard the M.V. Polar Queen, research vessel. The main objectives of the expedition were a) Basement: ...


99. Geological mapping and investigations of the rock groups in the area of the Mariner Glacier, North Victoria Land [K002_1966_1967_NZ_1]
The area around the Mariner Glacier was investigated to make a geological survey of the whole section, and in particular, to ascertain the relationship and contact between the sedimentary rocks known ...


100. Geological mapping and measurements of the Priestley Formation and granite-metasedimentary rocks of the Preistly and Campbell Glacier region, Terra Nova Bay [K002_1982_1983_NZ_1]
The Southern Deep Freeze Range, Northern Foothills and Inexpressible Island in North Victoria Land, have been geologically investigated in the past. The granites of this area belong to a completely ...


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