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Bengal Fan

Copeland P. and Harrison T. M. (1990) Episodic rapid uplift in the Himalaya revealed by Ar/ Ar analysis of detrital K-feldspar and muscovite, Bengal Fan. Geology 18, 354-357. [Pg.1548]

Corrigan J. D. and Crowley K. D. (1992) Unroofing of the Himalayas a view from apatite fission-track analysis of Bengal Fan sediments. Geophys. Res. Lett. 19, 2345—2348. [Pg.1549]

Galy A., FranceLanord C., and Derry L. A. (1996) The Late OUgocene Early Miocene Himalayan belt constraints deduced from isotopic compositions of Early Miocene turbidites in the Bengal fan. Tectonophysics 260(1—3), 109-118. [Pg.3332]

France-Lanord C, Derry LA (1994) Delta C-13 of organic-carbon in the bengal fan-somce evolution and transport of C3 and C4 plant carbon to marine-sediments. Geochim Cosmochim Acta 58 4809-4814 Francey RJ, Steele LP, Langenfelds RL, Allison CE, Cooper LN, Dtmse BE, Bell BG, Mtrrray TD, Tail HS, Thompson L, Masarie KA (1998) Atmospheric carbon dioxide and its stable isotope ratios, methane, carbon monoxide, nitrous oxide and hydrogen from Shetland Isles. Atmospheric Environ 32 3331-3338... [Pg.599]

KL 11°10.9 N 88°24.9 E 3293 m 10.00 m Bengal Fan terrigenous olay, silt, sand foram. and nannofbssil ooze... [Pg.52]

Fig. 2.23 Parasound seismogram section recorded across an inactive meandering channel in the Bengal Fan. The sediments of the terrace were sampled by piston core 47KL marked by the black bar. Vertical exaggeration (VE) of sedimentary structures is 200. The ship s course is displayed above the seismogram section. The terrace exhibits features which might be interpreted as old buried channels. Modified after Breitzke (1997). Fig. 2.23 Parasound seismogram section recorded across an inactive meandering channel in the Bengal Fan. The sediments of the terrace were sampled by piston core 47KL marked by the black bar. Vertical exaggeration (VE) of sedimentary structures is 200. The ship s course is displayed above the seismogram section. The terrace exhibits features which might be interpreted as old buried channels. Modified after Breitzke (1997).
The fourth example from the distal Bengal Fan (Hiibscher et al. 1997) was recorded during RV Sonne craise S0125 and displays terrigenous features and sediments (Fig. 2.25d). Active and older abandoned channel levee systems are characterized by a diffuse reflection pattern which indicates sediments of coarse-grained turbidites. Signal penetration in such environments is rather low and reaches about 30 - 40 m. [Pg.64]

Hubscher C., SpieB V., Breitzke M., Weber M.E., 1997. The youngest channel-levee system of the Bengal Fan results from digital echosounder data. Marine Geology 141 125 - 145... [Pg.70]

Copeland P, Harrison TM, Heizler MT (1990) " °Ar/ Ar single-crystal dating of detrital muscovite and K-feldspar from Leg 116, Southern Bengal Fan Implications for the uplift and erosion of the Himalayas. Proc Ocean Drill Progr 116 93-114... [Pg.811]

Bachman, R.T., and Hamilton, E.L. 1982. Sediment sound velocity from sonobuoys Sunda Trench and forearc basins, Nicobar and Central Bengal fans, and Andaman Sea Basin. Journal of Geophysical Research, B86(ll) 9341-9346. [Pg.518]

See other pages where Bengal Fan is mentioned: [Pg.160]    [Pg.3310]    [Pg.3332]    [Pg.270]    [Pg.52]    [Pg.54]    [Pg.54]    [Pg.55]    [Pg.56]    [Pg.56]    [Pg.57]    [Pg.61]    [Pg.61]    [Pg.62]    [Pg.63]    [Pg.66]    [Pg.66]    [Pg.573]    [Pg.414]    [Pg.527]    [Pg.35]   
See also in sourсe #XX -- [ Pg.270 ]



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