Deep Sea Drilling Project Initial Reports Volume 35
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Thurston Island
RESEARCH ARTICLE Thurston Island (West Antarctica) Between Gondwana 10.1029/2018TC005150 Subduction and Continental Separation: A Multistage Key Points: • First apatite fission track and apatite Evolution Revealed by Apatite Thermochronology ‐ ‐ (U Th Sm)/He data of Thurston Maximilian Zundel1 , Cornelia Spiegel1, André Mehling1, Frank Lisker1 , Island constrain thermal evolution 2 3 3 since the Late Paleozoic Claus‐Dieter Hillenbrand , Patrick Monien , and Andreas Klügel • Basin development occurred on 1 2 Thurston Island during the Jurassic Department of Geosciences, Geodynamics of Polar Regions, University of Bremen, Bremen, Germany, British Antarctic and Early Cretaceous Survey, Cambridge, UK, 3Department of Geosciences, Petrology of the Ocean Crust, University of Bremen, Bremen, • ‐ Early to mid Cretaceous Germany convergence on Thurston Island was replaced at ~95 Ma by extension and continental breakup Abstract The first low‐temperature thermochronological data from Thurston Island, West Antarctica, ‐ fi Supporting Information: provide insights into the poorly constrained thermotectonic evolution of the paleo Paci c margin of • Supporting Information S1 Gondwana since the Late Paleozoic. Here we present the first apatite fission track and apatite (U‐Th‐Sm)/He data from Carboniferous to mid‐Cretaceous (meta‐) igneous rocks from the Thurston Island area. Thermal history modeling of apatite fission track dates of 145–92 Ma and apatite (U‐Th‐Sm)/He dates of 112–71 Correspondence to: Ma, in combination with kinematic indicators, geological -
Paleomagnetic Investigations in the Ellsworth Land Area, Antarctica
eastern half consists of gneiss (some banded), amphi- probably have mafic dikes as well as felsite dikes, are bolite, metavolcanics, granodiorite, diorite, and present. In the eastern part of the island, mafic dikes gabbro. Contacts are rare, and the relative ages of occur in banded gneiss. A dio rite- to-gabbroic mass is these rock bodies are in doubt. The Morgan Inlet present in the north central portion of the island. gneiss may represent the oldest rock on Thurston Granite-to-diorite bodies occur in the south central Island; earlier work (Craddock et al.. 1964) gave a portion of the island and contain "meta-volcanic" Rb-Sr age of 280 m.y. on biotite from this rock. rocks and mafic dikes. Granite-granodiorite-to-diorite Studies in the Jones Mountains were mainly on the rocks occur in the western portion of the island. This unconformity between the basement complex and the latter plutonic mass is probably the youngest body in overlying basaltic volcanic rocks to evaluate the evi- which mafic dikes are also present. About 10 miles dence for Tertiary glaciation. Volcanic strata just southwest of Thurston Island, a medium-grained above the unconformity contain abundant glass and granodiorite plutonic mass forms Dustin Island, pillow-like masses suggestive of interaction between where three samples were collected at Ehlers Knob. lava and ice. Tillites with faceted and striated exotic In the Jones Mountains, 27 oriented samples were pebbles and boulders are present in several localities collected from the area around Pillsbury Tower, on in the lower 10 m of the volcanic sequence. -
A Revised Geochronology of Thurston Island, West Antarctica and Correlations Along the Proto
1 A revised geochronology of Thurston Island, West Antarctica and correlations along the proto- 2 Pacific margin of Gondwana 3 4 5 6 T.R. Riley1, M.J. Flowerdew1,2, R.J. Pankhurst3, P.T. Leat1,4, I.L. Millar3, C.M. Fanning5 & M.J. 7 Whitehouse6 8 9 1British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK 10 2CASP, 181A Huntingdon Road, Cambridge, CB3 0DH, UK 11 3British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK 12 4Department of Geology, University of Leicester, Leicester, LE1 7RH, UK 13 5Research School of Earth Sciences, The Australian National University, Canberra ACT 0200, Australia 14 6Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden 15 16 17 18 19 20 21 22 23 24 *Author for correspondence 25 e-mail: [email protected] 26 Tel. 44 (0) 1223 221423 1 27 Abstract 28 The continental margin of Gondwana preserves a record of long-lived magmatism from the Andean 29 Cordillera to Australia. The crustal blocks of West Antarctica form part of this margin, with 30 Palaeozoic – Mesozoic magmatism particularly well preserved in the Antarctic Peninsula and Marie 31 Byrd Land. Magmatic events on the intervening Thurston Island crustal block are poorly defined, 32 which has hindered accurate correlations along the margin. Six samples are dated here using U-Pb 33 geochronology and cover the geological history on Thurston Island. The basement gneisses from 34 Morgan Inlet have a protolith age of 349 ± 2 Ma and correlate closely with the Devonian – 35 Carboniferous magmatism of Marie Byrd Land and New Zealand. -
Biological Survey of Ellsworth Land Waigreen Coast Were Investigated
29°S. 126°W., respectively. These ancient magnetic poles for West Antarctica are displaced from pole positions for rocks of similar age in East Antarctica (Fig. 1). Tes tiary dikes give a pole position of 62°S. 64°E., while Pleistocene volcanics give a pole position of 78°S. 128°W. The paleomagnetic data, especially the Cretaceous rocks, strongly suggest that East and West Antarctica are unrelated geologically or structur- ally. Schopf (1969), using an analysis of sea-floor spreading, indicates that the reconstruction of Gond- wanaland "would be simplified if West Antarctica is not regarded as Part of the ancient Antarctic crustal unit." Hamilton (1967) also suggests that the pre-Ter- tiary complexes of West Antarctica are "disconnected from each other and from the terranes of East Ant- arctica." Paleomagnetic data further demonstrate that Fig. 1. Walker Mountains, Thurston Island, looking northwestward West Antarctica is independent of the ancient ant- from 600-m elevation. Mount Dowling in left foreground. arctic unit. ciated studies in the Ellsworth Land Survey, was con- References ducted with helicopters from temporary base camps at Craddock, C., T. W. Bastien, and R. H. Rutford. 1964. the base of the King Peninsula and at the Jones Geology of the Jones Mountains area. In: Antarctic Geol- Mountains. ogy, North-Holland Publ. Co., Amsterdam, p. 171-187. Hamilton, W. 1967. Tectonics of Antarctica. Tectonophysics, Although laboratory analysis of the many samples 4(4-6) : 555. collected has not been completed, a summary of the Scharnberger, C., T. Early, 1-Chi Hsu, and LeRoy Sharon. field observations has been compiled (Table 1). -
19. Continental Rise and Abyssal Plain Sedimentation in the Southeast Pacific Basin — Leg 35 Deep Sea Drilling Project
19. CONTINENTAL RISE AND ABYSSAL PLAIN SEDIMENTATION IN THE SOUTHEAST PACIFIC BASIN — LEG 35 DEEP SEA DRILLING PROJECT Brian E. Tucholke,1 Charles D. Hollister,2 Fred M. Weaver,3 and Walter R. Vennum4 Somewhere hearts are happy, Somewhere children shout, But there'll be no joy in Mudville 'Til the Miocene gives out. —C. Craddock ABSTRACT Four sites were drilled on the Bellingshausen Abyssal Plain and continental rise off Antarctica during Leg 35 of the Deep Sea Drill- ing Project. Site 322 penetrated 513 meters of lower Miocene (? Oligocene) to Holocene diatomaceous claystone, siltstone, and sandstone overlying basalt. A similar Neogene section at Site 323 caps 63 meters of upper Maestrichtian to (?) Oligocene brown nan- no claystone and Fe-claystone bottoming on basalt. Site 324 pene- trated 218 meters of Pliocene-Pleistocene terrigenous clay with in- terbedded silt layers interpreted as contourites, and 718 meters of lower Miocene-Holocene diatomaceous claystone grading down- ward into coarse sandstone were drilled at Site 325. The brown Fe-claystone at Site 323 and a similar, thin basal unit at Site 322 indicate pelagic deposition, largely from volcanogenic sources at rates <0.5 cm/1000 yr, from the late Maestrichtian to the (?) Oligocene. Abundant nannoplankton in lower Paleocene clay- stone suggest depression of the CCD at this time, in contrast to a shallow CCD in most other areas of the world's oceans. Significant bottom-current activity was not initiated until the latest Oligocene or early Miocene, probably in response to formation of deep gaps in the Drake Passage area. An apparent 35-40 m.y. -
The Ellsworth Land Survey Erected and the Scientific Personnel Arrived
During the first week of November, Camp 1 was The Ellsworth Land Survey erected and the scientific personnel arrived. Bad weather prevented the start of work until November F. ALTON WADE 15, allowing only eight days in all for helicopter flying that month and December. Nevertheless, the Department of Geology and Geophysics efficiency of the helicopters allowed completion of the Texas Technological College necessary work from this camp, and some of the geol- and ogists returned to McMurdo December 16. On the CAMPBELL CRADDOCK same day, four Navy men were flown to the Jones Mountains to begin construction of Camp 2. Department of Geology The relieving scientific party made three unsuccess- University of Wisconsin ful flights to Camp 2 before weather conditions per- mitted landing on January 5. Camp equipment was During the 1966-1967 summer season, the United transferred on five C-130 flights, and Camp 1 was States began a multidisciplinary, helicopter-supported closed January 10 when the three helicopters flew to scientific survey of coastal West Antarctica. The pro- Camp 2. Helicopter operations in the Jones Moun- gram began near the Ross Ice Shelf in western Marie tains began January 11, and the month proved to be Byrd Land, and the original plan was to work east- a favorable one for working. Scientific work by either ward that season through a series of camps to the helicopter or motor toboggan was possible on two Eights Coast. The expected rate of progress was not days out of three, although the helicopters and 14 obtained, however, because of generally poor weather men were pinned down in Camp 1 January 13-17 and the limited number of flying days. -
The Geology of the Eights Coast Ar CAMPBELL CRADDOCK, CRAIG M
References Craddock, C., T. W. Bastien, and R. H. Rutford. 1964. Geology of the Jones Mountains. In: Antarctic Geology, North-Holland Pubi. Co., Amsterdam, p. 171-187. Rutford, R. H., C. Craddock, and T. W. Bastien. 1968. Late Tertiary Glaciation and Sea-Level Changes in Ant- arctica. Palaeo geography, Palaeoclinzatology, Palaeoecology, I 5(1): 15-39. The Geology of the Eights Coast Ar CAMPBELL CRADDOCK, CRAIG M. WHITE, Photo: K. E. La Prade and ROBERT H. RUTFORD USARP Jamesway building on King Peninsula six weeks after erection. Access is by a tunnel through the drift. Camp included Department of Geology and Geophysics three other .Jamesways. University of Wisconsin gist from the Instituto Antártico Chileno, Santiago Responsibility for the geological prograni during the dc Chile; and Boris Lopatin, basement geologist from latter part of the 1968-1969 Ellsworth Land Survey the Institute of Arctic Geology, , Leningrad, U.S.S.R. rested with our three-man party from the University Rocks of the Hudson Mountains and King Penin- of Wisconsin. Part of Thurston Island was studied by sula consist of olivine basalts and tuffs. Well-devel- White with helicopter support from Camp 1. All oped pillow lava occurs at Mount Nickens, but of us who worked in the Jones Mountains from Camp elsewhere the lavas occur as thick layers of scora- 2 used both helicopter and motor toboggan transport. ceous olivine basalts, typically interstratified with The remainder of the area was studied by Craddock tuffs. Volcanic rocks rest unconformably on basement and White in helicopters from Camp 2. rocks in the nearby Jones Mountains, but the contact All of the significant and accessible rock exposures is not exposed in the Hudson Mountains-King Penin- along the Eights Coast from Lepley Nunatak to sula areas. -
Abbot Ice Shelf, Structure of the Amundsen Sea Continental 10.1002/2014GC005570 Margin and the Southern Boundary of the Bellingshausen Plate
PUBLICATIONS Geochemistry, Geophysics, Geosystems RESEARCH ARTICLE Abbot Ice Shelf, structure of the Amundsen Sea continental 10.1002/2014GC005570 margin and the southern boundary of the Bellingshausen Plate Key Points: seaward of West Antarctica Abbot Ice Shelf is underlain by E-W rift basins created at 90 Ma James R. Cochran1, Kirsty J. Tinto1, and Robin E. Bell1 Amundsen shelf shaped by subsidence, sedimentation, and 1Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York, USA passage of the ice sheet Bellingshausen plate boundary is located near the base of continental Abstract Inversion of NASA Operation IceBridge airborne gravity over the Abbot Ice Shelf in West Ant- slope and rise arctica for subice bathymetry defines an extensional terrain made up of east-west trending rift basins formed during the early stages of Antarctica/Zealandia rifting. Extension is minor, as rifting jumped north of Correspondence to: J. R. Cochran, Thurston Island early in the rifting process. The Amundsen Sea Embayment continental shelf west of the [email protected] rifted terrain is underlain by a deeper, more extensive sedimentary basin also formed during rifting between Antarctica and Zealandia. A well-defined boundary zone separates the mildly extended Abbot extensional Citation: terrain from the deeper Amundsen Embayment shelf basin. The shelf basin has an extension factor, b,of Cochran, J. R., K. J. Tinto, and R. E. Bell 1.5–1.7 with 80–100 km of extension occurring across an area now 250 km wide. Following this extension, (2015), Abbot Ice Shelf, structure of the Amundsen Sea continental margin and rifting centered north of the present shelf edge and proceeded to continental rupture. -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc) Volume 1-36: Feb 2019 Vessel Names Are Shown Viz: “Aconcagua”. S
ANTARCTIC1 Compiled by Mike Wing 12: 190, 19: 144, 22: 5, New Zealand Antarctic Society (Inc) Injury, 1: 340, 2: 118, 492, 3: 480, 509, 523, 4: 15, 8: 130, 282, 315, 317, 331, 409, Volume 1-36: Feb 2019 9: 12, 18, 19, 23, 125, 313, 394, 6: 17, 7: 6, 22, 11: 395, 12: 348, 18: 56, 19: 95, Vessel names are shown viz: “Aconcagua”. See also 22: 16, 32: 29, list of ship names under ‘Ships’. Ships All book reviews are shown under ‘Book Reviews’ ANARE, 8: 13, All Universities are shown under ‘Universities’ Argentine Navy, 1: 336, Aircraft types appear under ‘Aircraft’. “Bahia Paraiso” Obituaries & Tributes are shown under 'Obituaries', see Sinking 11: 384, 391, 441, 476, 12: 22, 200, also individual names. 353, 13: 28, Fishing, 30: 1, Vol 20 page numbers 27-36 are shared by both double Japanese, 24: 67, issues 1&2 and 3&4. Those in double issue 3&4 are NGO, 29, 62(issue 4), marked accordingly viz: 20: 4 (issue 3&4) Polar, 34, Soviet, 8: 426, Vol 27 page numbers 1-20 are shared by both issues Tourist ships, 20: 58, 62, 24: 67, 1&2. Those in issue 2 are marked accordingly viz. 27: Vehicles, (issue 2) NZ Snow-cat, 2: 118, US bulldozer, 1: 202, 340, 12: 54, Vol 29 pages 62-68 are shared by both issues 3&4. ACECRC, see Antarctic Climate & Ecosystems Duplicated pages in 4 are marked accordingly viz. 63: Cooperation Research Centre (issue 4). Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Ackroyd, Lieut. -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
ANTARCTIC 1 Compiled by Mike Wing Injury, 1: 340, 2: 118, 492, 3: 480, 509, 523, New Zealand Antarctic Society (Inc) 4: 15, 8: 130, 282, 315, 317, 331, 409, 9: 12, 18, 19, 23, 125, 313, 394, 6: 17, 7: 6, Volume 1-35: April 2018 22, 11: 395, 12: 348, 18: 56, 19: 95, 22: 16, 32: 29, Vessel names are shown viz: “Aconcagua” Ships All book reviews are shown under ‘Book Reviews’ ANARE, 8: 13, All Universities are shown under ‘Universities’ Argentine Navy, 1: 336, Aircraft types appear under Aircraft. Fishing, 30: 1, Obituaries & Tributes are shown under 'Obituaries', Japanese, 24: 67, see also individual names. NGO, 29, 62(issue 4), Polar, 34, Vol 20 page numbers 27-36 are shared by both Soviet, 8: 426, double issues 1&2 and 3&4. Those in double issue Tourist ships, 20: 58, 62, 24: 67, 3&4 are marked accordingly viz: 20: 4 (issue 3&4) Vehicles, NZ Snow-cat, 2: 118, Vol 27 page numbers 1-20 are shared by both issues US bulldozer, 1: 202, 340, 12: 54, 1&2. Those in issue 2 are marked accordingly viz. 27: ACECRC, see Antarctic Climate & Ecosystems (issue 2) Cooperation Research Centre Acevedo, Capitan. A.O. 4: 36, Vol 29 pages 62-68 are shared by both issues 3&4. Ackerman, Piers, 21: 16, Duplicated pages in 4 are marked accordingly viz. 63: Ackroyd, Lieut. F: 1: 307, (issue 4). Ackroyd-Kelly, J. W., 10: 279, Acland, D, 31: 30 “Aconcagua”, 1: 261 Acta Palaeontolegica Polonica, 25: 64, A ACZP, see Antarctic Convergence Zone Project Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, “101 In Sung”, f/v, 21: 36, Adams, Chris, 11: 198, 274, 12: 331, 396, A-Frame Hut – see Scott Base Adams, David Hempleman, 29: 60, ‘A’ Hut (TAE) – see Scott Base Adams, Dieter, 12: 294, “Aaron” r/v, 30:1, 45, Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Aaron, Edwin, 11: 55, Adams, J.B., 26: 22, Abbiss, Jane, 20: 8, Adams, Lt. -
Text to Accompany Map I-2600-E
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I–2600–E U.S. GEOLOGICAL SURVEY COASTAL-CHANGE AND GLACIOLOGICAL MAP OF THE EIGHTS COAST AREA, ANTARCTICA: 1972–2001 By Charles Swithinbank,1 Richard S. Williams, Jr.,2 Jane G. Ferrigno,3 Kevin M. Foley,3 Christine E. Rosanova,4 and Lina M. Dailide5 INTRODUCTION Ferrigno, 1988). The project was later modified to include Landsat 4 and 5 MSS and Thematic Mapper (TM) (and in some Background areas Landsat 7 Enhanced Thematic Mapper Plus (ETM+)), Changes in the area and volume of polar ice sheets are intri RADARSAT images, and other data where available, to compare cately linked to changes in global climate, and the resulting changes during a 20- to 25- or 30-year time interval (or longer changes in sea level may severely impact the densely populated where data were available, as in the Antarctic Peninsula). The coastal regions on Earth. Melting of the West Antarctic part results of the analysis are being used to produce a digital database alone of the Antarctic ice sheet could cause a sea-level rise of and a series of USGS Geologic Investigations Series Maps approximately 6 meters (m). The potential sea-level rise after (I–2600) consisting of 24 maps at 1:1,000,000 scale and 1 map melting of the entire Antarctic ice sheet is estimated to be 65 m at 1:5,000,000 scale, in both paper and digital format (Williams (Lythe and others, 2001) to 73 m (Williams and Hall, 1993). In and others, 1995; Williams and Ferrigno, 1998; Ferrigno and spite of its importance, the mass balance (the net volumetric gain others, 2002). -
Implications for the Tectonics of West Antarctica
JOURNALOF GEOPHYSICALRESEARCH, VOL. 96, NO. Bll, PAGES17,935-17,954, OCTOBER 10, 1991 New PaleomagneticData FromThurston Island' Implications for the Tectonicsof West Antarcticaand Weddell Sea Opening A.M. GRUNOW1 ByrdPolar Research Center, Ohio State University, Columbus Lamont-DohertyGeological Observatory andthe Department ofGeological Sciences, Columbia University, New York I. W. D. D ALZlEL Institutefor Geophysics,University of Texasat Austin Palcomagneticdata from threeWest Antarcticcrustal blocks (Antarctic Peninsula (AP), ThurstonIsland-Eights Coast (TI), and the Ellsworth-Whitmore Mountains (EWM) indicate that there has been motion between the individualblocks and motion relative to EastAntarctica during the Mesozoic. A Triassicpalcomagnetic pole from theTI block(116øE, 61øS, A95 = 19.4ø,N = 3 VGPs)appears toindicate that the block has rotated -90 ørelative to EastAntarctica between 230 Ma and110 Ma. Ourpreviously reported Middle Jurassic palcomagnetic pole from the EWM block indicates that a 90 ø rotation relative to East Antarctica occurred sometime between the Cambrian and 175 Ma. We believe that the 90 ø counterclockwise EWM rotation occurred between-220 Ma and 175 Ma related to thedevelopment of post-GondwanideOrogeny shear zones. The motion of theAP, TI, andEWM blocksappears to be linked duringthe mid- to late Mesozoicto threemajor events in the evolutionof the southemocean basins. Openingin theMozambique-Somali-Weddell Sea basins may have produced major counterclockwise rotation of the TI blockwith respectto EastAntarctica between the Jurassic and Early Cretaceousbased on new LateJurassic (145øE,64.5øS, A95 = 7ø,N= 5 VGPs)poles. We believe that the TI rotation,as well as deformation inthe southem AP block, wascaused by collisionand shearingof the EWM blockagainst the othertwo asthe EWM block moved southwardwith East Antarctica.