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Identification of greigite in lake sediments and its magnetic significance

         

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[1]Xue, B., Wang, S., Xia, W. et al., The uplift and environmental change of Qinghai-Xizang (Tibetan) Plateau in the past 0.9 Ma inferred from Core RM in Zoigê Basin, Science in China, Ser. D, 1998, 41(2): 165-170.[2]Hoffmann, V., Greigite (Fe3S4): magnetic properties and first domain observations, Phys. Earth Planet Inter., 1992, 70: 288-301.[3]Snowball, I., Thompson, R., A stable chemical remanence in Holocene sediments, J. Geophys. Res., 1990, 95: 4471-4479.[4]Dekkers, M. J., Magnetic properties of natural pyrrhotite, II: High- and low-temperature behaviour of Jrs and TRM as function of grain size, Phys. Earth Planet Inter., 1989, 57: 266-283.[5]Rochette, P., Fillion, G., Mattéi, J. L. et al., Magnetic transition at 30 - 234 K in pyrrhotite: insight into a widespread occurrence of this mineral in rocks, Earth Planet Sci. Lett., 1990, 98: 319-328.[6]McCabe, C., Channell, J. E. T., Late Paleozoic remagnetization in limestones of the Craven Basin (northern England) and the rock magnetic fingerprint of remagnetized sedimentary carbonates, J. Geophys. Res., 1994, 99: 4603-4612.[7]Snyder, R. L., Analytical profile fitting of X-ray powder diffraction profiles in Rietveld analysis, in The Rietveld Method (ed., R. A. Young), Oxford: Oxford University Press, 1995, 111-131.[8]Klug, H. P., Alexander, L. E., X-ray Diffraction Procedures for Polycrystalline and Amorphous Materials, New York: Illus. John Wiley & Sons, 1954, 97.[9]Diaz, I. J. C., Kirschvink, L., Magnetic domain state and coercivity predictions for biogenic greigite (Fe3S4): A comparison of theory with magnetosome observations, J. Geophys. Res., 1992, 97: 309-315.[10]Snowball, I., Thompson, R., The occurrence of greigite in sediments from Loch Lomond, J. Quatern. Sci., 1988, 3: 121-125.[11]Ariztegui, D., Dobson, J., Magnetic investigations of framboidal greigite formation; a record of anthropogenic environmental changes in eutrophic Lake St. Moritz, Switzerland, The Holocene, 1996, 6: 235-241[12]Hallam, D. F., Maher, B. A., A record of reversed polarity carried by the iron sulphide greigite in British early Pleistocene sediments, Earth Planet. Sci. Lett., 1994, 121: 71-80.[13]Sagnotti, L., Winkler, A., Rock magnetism and palaeomagnetism of greigite-bearing mudstones in the Italian peninsula, Earth Planet. Sci. Lett., 1999, 165(1): 67-80.[14]Hu, S., Appel, E., Wang, S., A magnetic study on lacustrine sediments from Zoige Basin, Eastern Tibetan Plateau, China: Magnetostratigraphy and environmental implications, Physics and Chemistry of the Earth (A), 1999, 24(9): 811-816.[15]Hu, S., Wang, S., Appel, E., Remanence acquisition and alteration in lake sediments, Chinese Sci. Bull., 1998, 43(17): 1421-1434.[16]Verosub, K. L., Roberts, A. P., Environmental magnetism: Past, present and future, J. Geophys. Res., 1995, 100: 2175-2192.[17]Wu, J., Wang, S., Climatic variation during the last interglacial period recorded in the lake carbonate deposit, eastern Qingzang Plateau, Chinese Sci. Bull., 1997, 42(12): 1017-1020.[18]Wu, J., Wang, S., Pan, H. et al., The palaeoclimatic characteristics since last 140 ka recorded in lacustrine isotopic carbonate in Core RM from eastern Tibetan Plateau, Science in China, Ser. D, 1997, 40(4): 443-448.

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