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- W2931536313 abstract "Abstract The Bengal Fan provides a Neogene record of Eastern and Central Himalaya exhumation. We provide the first detrital thermochronological study (apatite and rutile U-Pb, mica Ar-Ar, zircon fission track) of sediment samples collected during International Ocean Discovery Program (IODP) Expedition 354 to the mid–Bengal Fan. Our data from rutile and zircon fission-track thermochronometry show a shift in lag times over the interval 5.59–3.47 Ma. The oldest sample with a lag time of <1 m.y. has a depositional age between 3.76 and 3.47 Ma, and these short lag times continue to be recorded upward in the core to the youngest sediments analyzed, deposited at <1 Ma. We interpret the earliest record of short lag times to represent the onset of extremely rapid exhumation of the Eastern Himalayan syntaxial massif, defined as the syntaxial region north of the Nam La Thrust. Below the interval characterized by short lag times, the youngest sample analyzed with long lag times (>6 m.y.) has a depositional age of 5.59–4.50 Ma, and the zircon and rutile populations then show a static peak until >12 Ma. This interval, from 5.59–4.50 Ma to >12 Ma, is most easily interpreted as recording passive erosion of the Greater Himalaya. However, single grains with lag times of <4 m.y., but with high analytical uncertainty, are recorded over this interval. For sediments older than 10 Ma, these grains were derived from the Greater Himalaya, which was exhuming rapidly until ca. 14 Ma. In sediments younger than 10 Ma, these grains could represent slower, yet still rapid, exhumation of the syntaxial antiform to the south of the massif. Lag times <1 m.y. are again recorded from 14.5 Ma to the base of the studied section at 17 Ma, reflecting a period of Greater Himalayan rapid exhumation. Mica 40Ar/39Ar and apatite U-Pb data are not sensitive to syntaxial exhumation: We ascribe this to the paucity of white mica in syntaxial lithologies, and to high levels of common Pb, resulting in U-Pb ages associated with unacceptably high uncertainties, respectively." @default.
- W2931536313 created "2019-04-11" @default.
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- W2931536313 date "2019-03-29" @default.
- W2931536313 modified "2023-10-16" @default.
- W2931536313 title "Spatial and temporal trends in exhumation of the Eastern Himalaya and syntaxis as determined from a multitechnique detrital thermochronological study of the Bengal Fan" @default.
- W2931536313 cites W1501514800 @default.
- W2931536313 cites W1524459215 @default.
- W2931536313 cites W1582364594 @default.
- W2931536313 cites W1606193387 @default.
- W2931536313 cites W1649405128 @default.
- W2931536313 cites W1817883290 @default.
- W2931536313 cites W1820519016 @default.
- W2931536313 cites W1851003657 @default.
- W2931536313 cites W1945261828 @default.
- W2931536313 cites W1945774637 @default.
- W2931536313 cites W1964319225 @default.
- W2931536313 cites W1965335989 @default.
- W2931536313 cites W1970369754 @default.
- W2931536313 cites W1977539321 @default.
- W2931536313 cites W1979219677 @default.
- W2931536313 cites W1984744627 @default.
- W2931536313 cites W2006664521 @default.
- W2931536313 cites W2007105153 @default.
- W2931536313 cites W2009732140 @default.
- W2931536313 cites W2019854791 @default.
- W2931536313 cites W2020159892 @default.
- W2931536313 cites W2020803911 @default.
- W2931536313 cites W2027774423 @default.
- W2931536313 cites W2031242600 @default.
- W2931536313 cites W2032196651 @default.
- W2931536313 cites W2036530612 @default.
- W2931536313 cites W2036810996 @default.
- W2931536313 cites W2037664285 @default.
- W2931536313 cites W2038890966 @default.
- W2931536313 cites W2041080687 @default.
- W2931536313 cites W2046809141 @default.
- W2931536313 cites W2048875731 @default.
- W2931536313 cites W2049330576 @default.
- W2931536313 cites W2054328333 @default.
- W2931536313 cites W2054541681 @default.
- W2931536313 cites W2054653182 @default.
- W2931536313 cites W2055356153 @default.
- W2931536313 cites W2058060439 @default.
- W2931536313 cites W2059653811 @default.
- W2931536313 cites W2063171135 @default.
- W2931536313 cites W2066857664 @default.
- W2931536313 cites W2067410203 @default.
- W2931536313 cites W2067990600 @default.
- W2931536313 cites W2068705742 @default.
- W2931536313 cites W2071737204 @default.
- W2931536313 cites W2073143625 @default.
- W2931536313 cites W2081866917 @default.
- W2931536313 cites W2089507620 @default.
- W2931536313 cites W2093041656 @default.
- W2931536313 cites W2096907895 @default.
- W2931536313 cites W2103258790 @default.
- W2931536313 cites W2103651454 @default.
- W2931536313 cites W2104654533 @default.
- W2931536313 cites W2110179328 @default.
- W2931536313 cites W2112767229 @default.
- W2931536313 cites W2115422262 @default.
- W2931536313 cites W2124299111 @default.
- W2931536313 cites W2126347797 @default.
- W2931536313 cites W2126427530 @default.
- W2931536313 cites W2127399890 @default.
- W2931536313 cites W2130801795 @default.
- W2931536313 cites W2137741292 @default.
- W2931536313 cites W2138410761 @default.
- W2931536313 cites W2139808875 @default.
- W2931536313 cites W2140972267 @default.
- W2931536313 cites W2145139483 @default.
- W2931536313 cites W2145709911 @default.
- W2931536313 cites W2146384001 @default.
- W2931536313 cites W2150884838 @default.
- W2931536313 cites W2152330090 @default.
- W2931536313 cites W2153038124 @default.
- W2931536313 cites W2159173511 @default.
- W2931536313 cites W2163166398 @default.
- W2931536313 cites W2165653118 @default.
- W2931536313 cites W2165681180 @default.
- W2931536313 cites W2168976981 @default.
- W2931536313 cites W2169517779 @default.
- W2931536313 cites W2186897992 @default.
- W2931536313 cites W2187680438 @default.
- W2931536313 cites W2194700010 @default.
- W2931536313 cites W2342638531 @default.
- W2931536313 cites W2344225269 @default.
- W2931536313 cites W2389698457 @default.
- W2931536313 cites W2476775448 @default.
- W2931536313 cites W2490144373 @default.
- W2931536313 cites W2493476472 @default.