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Southeast Indian Ocean

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Journal Article
Published: 31 October 2022
Journal of Foraminiferal Research (2022) 52 (4): 248–263.
... been conducted in the southeast Indian Ocean ( Boltovskoy 1974a , 1974b for DSDP Leg 26; Akers 1974a , 1974b , and Rögl, 1974 for DSDP Leg 27, Site 262). Excepting a few, all these studies were mainly taxonomic and lacked integration with magnetostratigraphic data from the Southeast Indian Ocean...
Journal Article
Published: 01 July 2008
Journal of Foraminiferal Research (2008) 38 (3): 251–270.
...Devesh K. Sinha; Ashutosh Kumar Singh Abstract The late Neogene section of ODP Hole 763A, Exmouth Plateau, southeast Indian Ocean, has been biostratigraphically subdivided into eight planktic foraminiferal zones. The zones are similar to those of the tropical northern Indian and tropical western...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1992
AAPG Bulletin (1992) 76 (7): 1034–1036.
... , v. 133 , 1485 p. Driscoll , N. W. , J. K. Weissel , G. D. Karner , and G. S. Mountain , 1991 , Stratigraphic response of a carbonate platform to relative sea level changes : Broken Ridge, southeast Indian Ocean: AAPG Bulletin , v. 75 , p. 808 - 831 . Droxler...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1992
AAPG Bulletin (1992) 76 (7): 1037–1041.
... slope : AAPG Bulletin , v. 69 , p. 1133 - 1144 . Driscoll , N. W. , J. K. Weissel , G. D. Karner , and G. S. Mountain , 1991 , Stratigraphic response of a carbonate platform to relative sea level changes : Broken Ridge, southeast Indian Ocean: AAPG Bulletin , v. 75 , p...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1991
AAPG Bulletin (1991) 75 (4): 808–831.
... level rise, and thus require minor modification in order to predict the development of the prograding clinoforms. Broken Ridge and Kerguelen-Heard Plateau, both located in the southeast Indian Ocean, appear to be conjugate rifted margins of a preexisting, submarine platform ( Figure 1 ) ( Mutter...
FIGURES | View All (22)
Journal Article
Journal: GSA Bulletin
Published: 01 February 1985
GSA Bulletin (1985) 96 (2): 176–189.
...DOUGLAS F. WILLIAMS; NANCY HEALY-WILLIAMS; PAMELA LESCHAK Abstract A quantitative study of the planktonic foraminiferal fauna and various related parameters in more than 100 surface sediment samples from the Southeast Indian Ocean has identified the major relationships which can be utilized...
Journal Article
Journal: GSA Bulletin
Published: 01 February 1985
GSA Bulletin (1985) 96 (2): 190–202.
...DOUGLAS F. WILLIAMS; DAVID GRIBBLE; NANCY HEALY-WILLIAMS; PAMELA LESCHAK Abstract Calcium carbonate dissolution patterns were determined for portions of the past 2.5 m.y. in 9 Eltanin piston cores distributed along the Southeast Indian Ridge in the Southeast Indian Ocean. Oxygen isotope...
Journal Article
Journal: GSA Bulletin
Published: 01 November 1983
GSA Bulletin (1983) 94 (11): 1345–1358.
...NOEL I. OSBORN; PAUL F. CIESIELSKI; MICHAEL T. LEDBETTER Abstract Biostratigraphy and magnetostratigraphy are used to identify deep-sea disconformities in the southeast Indian Ocean. The hiatuses are used to define periods of increased bottom-water activity and to indicate deep-sea circulation...
Journal Article
Published: 01 January 1979
Micropaleontology (1979) 25 (1): 1–19.
Journal Article
Published: 01 January 1979
Journal of Foraminiferal Research (1979) 9 (1): 50–60.
Journal Article
Journal: GSA Bulletin
Published: 01 October 1976
GSA Bulletin (1976) 87 (10): 1529–1531.
Journal Article
Journal: GSA Bulletin
Published: 01 October 1976
GSA Bulletin (1976) 87 (10): 1531–1532.
Journal Article
Journal: GSA Bulletin
Published: 01 August 1975
GSA Bulletin (1975) 86 (8): 1058–1066.
...RICHARD G. BLANK; STANLEY V. MARGOLIS Abstract Sediment and microfossils from three subantarctic deep-sea cores recovered in the Southeast Indian Ocean have revealed a detailed climatic and glacial history for the Pliocene Epoch. Two cores contain sediment sequences that overlap and are of middle...
Image
(A) Bathymetry of the Southeast Indian Ocean is shown. Black solid lines mark mid-ocean ridges. Thin gray solid lines are isochrons at 10 m.y. intervals. Red circles with black borders show hotspots. Fracture zones (FZs) are labeled as AFZ—Amsterdam Fracture Zone, BFZ—Balleny Fracture Zone, GEFZ—George V Fracture Zone, GFZ—Geelvinck Fracture Zone, and TFZ—Tasman Fracture Zone. Other abbreviations: AAD—Australian-Antarctic Discordance, ANT—Antarctica, AUS—Australia, BR—Broken Ridge, KP—Kerguelen Plateau, MTJ—Macquarie triple junction, PAC—Pacific, PAR—Pacific-Antarctic Ridge, RTJ—Rodrigues triple junction, and SEIR—Southeast Indian Ridge. (B) Satellite-derived free air gravity anomaly data. (C) Sediment thickness. (D) Oceanic crustal age. (E) Calculated mantle Bouguer anomaly (MBA). (F) Dynamic topography from Flament et al. (2013).
Published: 09 October 2020
Figure 1. (A) Bathymetry of the Southeast Indian Ocean is shown. Black solid lines mark mid-ocean ridges. Thin gray solid lines are isochrons at 10 m.y. intervals. Red circles with black borders show hotspots. Fracture zones (FZs) are labeled as AFZ—Amsterdam Fracture Zone, BFZ—Balleny Fracture
Image
Plate motion of the Southeast Indian Ocean since 50 Ma from the revised global plate model (version 1.14) of Müller et al. (2016) is shown. Color boxes mark on-axis Phoenix slab material that has been drawn up from the mantle transition zone by the spreading Southeast Indian Ridge, causing the symmetric v-shaped, low residual bathymetry anomaly and other anomalies. Transparent filled areas mark locations of the Southeast Indian Slab (SEIS) at the mantle transition zone depth, which has been migrating northward in concert with the mid-ocean ridge and leaves an off-axis “cold slab” track. AAD—Australian-Antarctic Discordance, SEIR—Southeast Indian Ridge.
Published: 09 October 2020
Figure 9. Plate motion of the Southeast Indian Ocean since 50 Ma from the revised global plate model (version 1.14) of Müller et al. (2016) is shown. Color boxes mark on-axis Phoenix slab material that has been drawn up from the mantle transition zone by the spreading Southeast Indian Ridge
Image
(A) Bathymetry of the Southeast Indian Ocean is shown. Black solid lines mark mid-ocean ridges. Thin gray solid lines are isochrons at 10 m.y. intervals. Red circles with black borders show hotspots. Fracture zones (FZs) are labeled as AFZ—Amsterdam Fracture Zone, BFZ—Balleny Fracture Zone, GEFZ—George V Fracture Zone, GFZ—Geelvinck Fracture Zone, and TFZ—Tasman Fracture Zone. Other abbreviations: AAD—Australian-Antarctic Discordance, ANT—Antarctica, AUS—Australia, BR—Broken Ridge, KP—Kerguelen Plateau, MTJ—Macquarie triple junction, PAC—Pacific, PAR—Pacific-Antarctic Ridge, RTJ—Rodrigues triple junction, and SEIR—Southeast Indian Ridge. (B) Satellite-derived free air gravity anomaly data. (C) Sediment thickness. (D) Oceanic crustal age. (E) Calculated mantle Bouguer anomaly (MBA). (F) Dynamic topography from Flament et al. (2013).
Published: 09 October 2020
Figure 1. (A) Bathymetry of the Southeast Indian Ocean is shown. Black solid lines mark mid-ocean ridges. Thin gray solid lines are isochrons at 10 m.y. intervals. Red circles with black borders show hotspots. Fracture zones (FZs) are labeled as AFZ—Amsterdam Fracture Zone, BFZ—Balleny Fracture
Image
—(a) Seasat image of regional sea-floor structures, southeast Indian Ocean and Tasman Sea adjacent to southeastern part of Australian continent. In Tasman Sea, Seasat image tends to confirm orientation of synthetic fracture zones derived from Weissel and Hayes’ (1977) analysis of this region. Tasman Sea is sharply separated from tectonic province of north-south fracture zones formed at Indo-Australian spreading axis by line extending southeast from Tasmania. Box shows area of (b). (b) High-resolution image of Bass basin (dotted line) and surrounding area. Image formed by use of high-pass filter and allocating spectrum to local value range. White line shows seismic line 11 (Williamson et al, 1987), Bl = test well 1 Bass, (c) Line drawing of portion of seismic line 11 (Williamson et al, 1987) showing local, intrasectional volcanics (black) encountered in test well 1 Bass. Volcanics are too thin to contribute to regional gravity signal, but prevent transmission of seismic pulse and, if susceptible, produce false basementdepth values using magnetics. Well symbols: empty circle = dry, abandoned well; half-filled circle = well with show of oil and gas, abandoned well; filled circle = oil and gas discovery well, (d) Continental margin of northwestern Australia. Seasat image made using mild edge filter and allocating color spectrum to shallow-water area. White box shows area of marine magnetic survey (Willcox, 1981). Thick dashes show locus of alignment apparent on regional images of northwestern Australia interpreted as master fracture zone (see text), which passes between Wombat plateau and Joey Rise (not on image) and northbounds Exmouth plateau.
Published: 01 September 1989
Figure 5 —(a) Seasat image of regional sea-floor structures, southeast Indian Ocean and Tasman Sea adjacent to southeastern part of Australian continent. In Tasman Sea, Seasat image tends to confirm orientation of synthetic fracture zones derived from Weissel and Hayes’ (1977) analysis
Journal Article
Journal: GSA Bulletin
Published: 01 March 1976
GSA Bulletin (1976) 87 (3): 321–339.
...J. P. KENNETT; N. D. WATKINS Abstract A large collection of USNS Eltanin deep-sea sedimentary cores and bottom photographs from the southeast Indian Ocean between long 70°E and 120°E, and between Antarctica and lat 30°S, were analyzed. Cores from the crest and flanks of the mid-ocean ridge...
Journal Article
Journal: GSA Bulletin
Published: 01 July 1976
GSA Bulletin (1976) 87 (7): 994–1002.
...DENNIS E. HAYES Abstract Asymmetric sea-floor spreading has occurred south of Australia within narrow longitudinal zones of the Southeast Indian Ocean. The process of asymmetric spreading can be shown to be continuous at the scale of about 10 km or less in contrast to a process involving large...
Journal Article
Journal: GSA Bulletin
Published: 09 October 2020
GSA Bulletin (2021) 133 (5-6): 1057–1070.
...Figure 1. (A) Bathymetry of the Southeast Indian Ocean is shown. Black solid lines mark mid-ocean ridges. Thin gray solid lines are isochrons at 10 m.y. intervals. Red circles with black borders show hotspots. Fracture zones (FZs) are labeled as AFZ—Amsterdam Fracture Zone, BFZ—Balleny Fracture...
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