Regional variations in magnetic properties of surface sediments in the Qaidam Basin and their paleoenvironmental implications
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X. Fang | M. Yan | Dawen Zhang | J. Zan | Zhiguo Zhang
[1] E. Appel,et al. Environmental implications of the magnetic record in Pleistocene lacustrine sediments of the Qaidam Basin, NE Tibetan Plateau , 2013 .
[2] P. Kapp,et al. Wind as the primary driver of erosion in the Qaidam Basin, China , 2013 .
[3] L. Ding,et al. Climatic and tectonic controls on sedimentation and erosion during the pliocene-quaternary in the qaidam basin (China) , 2013 .
[4] E. Wang,et al. Cenozoic tectonic evolution of the Elashan range and its surroundings, northern Tibetan Plateau as constrained by paleomagnetism and apatite fission track analyses , 2012 .
[5] Weijian Zhou,et al. Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka , 2012, Scientific Reports.
[6] E. Appel,et al. Paleoclimatic implications of magnetic susceptibility in Late Pliocene-Quaternary sediments from deep drilling core SG-1 in the western Qaidam Basin (NE Tibetan Plateau) , 2012 .
[7] Gang Zhang,et al. Quantitative assessment on the cloning efficiencies of lentiviral transfer vectors with a unique clone site , 2012, Scientific Reports.
[8] Michael E. Evans,et al. Environmental Magnetism: Principles and Applications of Enviromagnetics , 2012 .
[9] J. Pelletier,et al. Wind erosion in the Qaidam basin, central Asia: Implications for tectonics, paleoclimate, and the source of the Loess Plateau , 2011 .
[10] R. Egli,et al. Consistent grain size distribution of pedogenic maghemite of surface soils and Miocene loessic soils on the Chinese Loess Plateau , 2010 .
[11] S. Xiong,et al. Magnetostratigraphy of the Dahonggou section, northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault , 2009 .
[12] A. Yin,et al. Cenozoic tectonic evolution of the Qaidam basin and its surrounding regions (Part 3): Structural geology, sedimentation, and regional tectonic reconstruction , 2008 .
[13] H. Birks,et al. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history , 2008 .
[14] J. King,et al. High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau , 2007 .
[15] J. Torrent,et al. Review of recent developments in mineral magnetism of the Chinese loess , 2007 .
[16] J. Bloemendal,et al. Rock magnetism and geochemistry of two plio-pleistocene Chinese loess-palaeosol sequences—implications for quantitative palaeoprecipitation reconstruction , 2005 .
[17] Tien-Nan Yang,et al. Magnetostratigraphy of Paleogene sediments from northern Qaidam Basin, China: Implications for tectonic uplift and block rotation in northern Tibetan plateau , 2005 .
[18] Yu Wang,et al. 40Ar/39Ar thermochronological evidence for formation and Mesozoic evolution of the northern-central segment of the Altyn Tagh fault system in the northern Tibetan Plateau , 2005 .
[19] F. Neubauer,et al. Sandstone provenance of north-western sectors of the intracontinental Cenozoic Qaidam basin, western China: Tectonic vs. climatic control , 2005 .
[20] M. Strecker,et al. Formation of internally drained contractional basins by aridity-limited bedrock incision , 2002 .
[21] D. Dunlop. Theory and application of the Day plot (Mrs/Ms versus Hcr/Hc) 1. Theoretical curves and tests using titanomagnetite data , 2002 .
[22] M. J. Singer,et al. Paleoclimatic significance of the temperature‐dependent susceptibility of Holocene Loess along a NW‐SE transect in the Chinese Loess Plateau , 2000 .
[23] M. Dekkers,et al. Low-Temperature Oxidation of Magnetite in Loess-Paleosol Sequences: a Correction of Rock Magnetic Parameters , 1999 .
[24] Yongxin Pan,et al. Magnetic proxy climate results from the Duanjiapo loess section, southernmost extremity of the Chinese loess plateau , 1999 .
[25] Wang Yongjin,et al. Magnetostratigraphy and sedimentologically derived geochronology of the Quaternary lacustrine deposits of a 3000 m thick sequence in the central Qaidam basin, western China , 1998 .
[26] David J. Dunlop,et al. Rock Magnetism: Fundamentals and Frontiers , 1997 .
[27] Roy Thompson,et al. Paleoclimatic Significance of the Mineral Magnetic Record of the Chinese Loess and Paleosols , 1992, Quaternary Research.
[28] J. T. Wang,et al. Partly pedogenic origin of magnetic variations in Chinese loess , 1990, Nature.
[29] J. King,et al. A comparison of different magnetic methods for determining the relative grain size of magnetite in natural materials: Some results from lake sediments , 1982 .