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Curray, JR.  1956.  The Analysis of 2-Dimensional Orientation Data. Journal of Geology. 64:117-&.Website
Curray, JR.  2014.  The Bengal Depositional System: From rift to orogeny. Marine Geology. 352:59-69.   10.1016/j.margeo.2014.02.001   AbstractWebsite

The Bengal Depositional System is defined as the surface depositional environments and the underlying sediment accumulation extending from the alluvial, lacustrine and paludal sediments of the lower Ganges and Brahmaputra Rivers, across the Bengal Delta, the Bangladesh continental shelf and slope to and including the Bengal Fan. Together it is one of the greatest sediment accumulations in the modern world, and is comparable in volume to the great sediment accumulations of the geological past. The history of formation started with the Mesozoic breakup of Eastern Gondwanaland, the northward drift of India, its collision with the southern margin of Asia, rotation and bending of the western Sunda Arc, and the penetration of the Indian continental mass into southern Asia. During this history, the regional tectonics evolved and sources and provenance of the sediments changed with the ultimate uplift of the Tibetan Plateau and the Himalayas. (C) 2014 Elsevier B.V. All rights reserved.

Curray, JR, Emmel FJ, Moore DG.  2002.  The Bengal Fan: morphology, geometry, stratigraphy, history and processes. Marine and Petroleum Geology. 19:1191-1223.   10.1016/s0264-8172(03)00035-7   AbstractWebsite

The Bengal Fan is the largest submarine fan in the world, with a length of about 3000 km, a width of about 1000 km and a maximum thickness of 16.5 km. It has been formed as a direct result of the India-Asia collision and uplift of the Himalayas and the Tibetan Plateau. It is currently supplied mainly by the confluent Ganges and Brahmaputra Rivers, with smaller contributions of sediment from several other large rivers in Bangladesh and India. The sedimentary section of the fan is subdivided by seismic stratigraphy by two unconformities which have been tentatively dated as upper Miocene and lower Eocene by long correlations from DSDP Leg 22 and ODP Legs 116 and 121. The upper Miocene unconformity is the time of onset of the diffuse plate edge or intraplate deformation in the southern or lower fan. The lower Eocene unconformity, a hiatus which increases in duration down the fan, is postulated to be the time of first deposition of the fan, starting at the base of the Bangladesh slope shortly after the initial India-Asia collision. The Quaternary of the upper fan comprises a section of enormous channel-levee complexes which were built on top of the preexisting fan surface during lowered sea level by very large turbidity currents. The Quaternary section of the upper fan can be subdivided by seismic stratigraphy into four subfans, which show lateral shifting as a function of the location of the submarine canyon supplying the turbidity currents and sediments. There was probably more than one active canyon at times during the Quaternary, but each one had only one active fan valley system and subfan at any given time. The fan currently has one submarine canyon source and one active fan valley system which extends the length of the active subfan. Since the Holocene rise in sea level, however, the head of the submarine canyon lies in a mid-shelf location, and the supply of sediment to the canyon and fan valley is greatly reduced from the huge supply which had existed during Pleistocene lowered sea level. Holocene turbidity currents are small and infrequent, and the active channel is partially filled in about the middle of the fan by deposition from these small turbidity currents. Channel migration within the fan valley system occurs by avulsion only in the upper fan and in the upper middle fan in the area of highest rates of deposition. Abandoned fan valleys are filled rapidly in the upper fan, but many open abandoned fan valleys are found on the lower fan. A sequence of time of activity of the important open channels is proposed, culminating with formation of the one currently active channel at about 12,000 years BP. (C) 2003 Elsevier Science Ltd. All rights reserved.

Paull, CK, Hecker B, Commeau R, Freemanlynde RP, Neumann C, Corso WP, Golubic S, Hook JE, Sikes E, Curray J.  1984.  Biological Communities at the Florida Escarpment Resemble Hydrothermal Vent Taxa. Science. 226:965-967.   10.1126/science.226.4677.965   Website
Shepard, FP, Curray JR.  1967.  Carbon-14 Determination of Sea Level Changes in Stable Areas. Progress in Oceanography. 4:283-&.Website
Moore, GF, Curray JR.  1981.  Characteristics of Sunda Subduction Zone. Aapg Bulletin-American Association of Petroleum Geologists. 65:959-960.Website
Curray, JR, Moore DG, Belderso.Rh, Stride AH.  1966.  Continental Margin of Western Europe - Slope Progradation and Erosion. Science. 154:265-&.   10.1126/science.154.3746.265   Website
Kelts, K, Einsele G, Curray J.  1981.  Controls on Diatomaceous Lithofacies in Obliquely Rifted Marginal Basin - Gulf of California. Aapg Bulletin-American Association of Petroleum Geologists. 65:945-945.Website
Henry, M, Raitt RW, Curray JR, Moore DG.  1975.  Delay-Time Function Analysis of Multiple Sonobouy Refraction Lines in Andaman Sea. Transactions-American Geophysical Union. 56:1063-1064.Website
Curray, JR, Emmel FJ.  1981.  Demise of the Diamantina Dent. Marine Geology. 40:M69-M72.   10.1016/0025-3227(81)90140-7   Website
Moore, DG, Curray JR, Emmel FJ.  1976.  Dynamic Processes of Upper Bengal Fan and Swatch of No Ground Canyon, Northeast Indian-Ocean. Aapg Bulletin-American Association of Petroleum Geologists. 60:699-699.Website
Moore, DG, Curray JR.  1982.  Geologic and Tectonic History of the Gulf of California. Initial Reports of the Deep Sea Drilling Project. 64:1279-1294.Website
Normark, WR, Curray JR.  1968.  Geology and Structure of Tip of Baja California Mexico. Geological Society of America Bulletin. 79:1589-&.   10.1130/0016-7606(1968)79[1589:gasott];2   Website
Stride, AH, Belderso.Rh, Curray JR, Moore DG.  1967.  Geophysical Evidence on Origin of Faeroe Bank Channel .I. Continuous Reflection Profiles. Deep-Sea Research. 14:1-&.   10.1016/0011-7471(67)90022-8   Website
Curray, JR, Moore DG.  1971.  Growth of Bengal Deep-Sea Fan and Denudation in Himalayas. Geological Society of America Bulletin. 82:563-&.   10.1130/0016-7606(1971)82[563:gotbdf];2   Website
Shepard, FP, Curray JR, Newman WA, Bloom AL, Newell ND, Tracey JI, Veeh HH.  1967.  Holocene Changes in Sea Level - Evidence in Micronesia. Science. 157:542-&.   10.1126/science.157.3788.542   Website
Kelts, K, Curray JR, Moore DG.  1982.  Introduction and Explanatory Notes. Initial Reports of the Deep Sea Drilling Project. 64:5-26.Website
Curray, JR, Moore DG.  1982.  Introduction to the Baja California Passive-Margin-Transect Symposium. Initial Reports of the Deep Sea Drilling Project. 64:1067-1069.Website
Curray, JR, Moore DG.  1982.  Introduction to the Guaymas Basin and Hydrothermal Symposium. Initial Reports of the Deep Sea Drilling Project. 64:1119-1121.Website
Curray, JR, Moore DG.  1982.  Introduction to the Guaymas Slope and Laminated Diatomite Symposium. Initial Reports of the Deep Sea Drilling Project. 64:1179-1181.Website
Einsele, G, Gieskes JM, Curray J, Moore DM, Aguayo E, Aubry MP, Fornari D, Guerrero J, Kastner M, Kelts K, Lyle M, Matoba Y, Molinacruz A, Niemitz J, Rueda J, Saunders A, Schrader H, Simoneit B, Vacquier V.  1980.  Intrusion of Basaltic Sills into Highly Porous Sediments, and Resulting Hydrothermal Activity. Nature. 283:441-445.   10.1038/283441a0   Website
Curray, JR.  1980.  Ipod Program on Passive Continental Margins. Philosophical Transactions of the Royal Society of London Series a-Mathematical Physical and Engineering Sciences. 294:17-33.   10.1098/rsta.1980.0008   Website