[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.
展开▼
机译:La fonction des identifications “comme si” dans un cas de psychose masquée↓A fun??o das identifica??es “como se” em um caso de psicose mascarada↓La función de las identificaciones “como si” en un caso de psicosis enmascarada↓Die Funktion der ?als ob“ Identifikationen in einem Fall maskierter Psychose↓在一个掩蔽精神病的情况,“好象”的识别作用
机译:识别从糠疹糠疹患者中分离的马拉色菌酵母菌种鉴定马德里na pit pit pit pit vers vers vers vers vers ser ser ser sul sul sul sul sul sul Bras Bras Bras Bras Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification Identification