Identifying sedimentation patterns in Lake Baikal using whole core and surface scanning magnetic suceptibility

[1]  P. Appleby,et al.  Mineral magnetic and physical properties of surficial sediments and onshore samples from the southern basin of Lake Baikal, Siberia , 1998 .

[2]  R. Flower.  Paleolimnology and recent environmental change in Lake Baikal: an introduction and overview of interrelated concurrent studies , 1998 .

[3]  A. Mackay,et al.  Sedimentary records of recent environmental change in Lake Baikal, Siberia , 1995 .

[4]  Vadim A. Kravchinsky,et al.  A rock-magnetic record from Lake Baikal, Siberia: Evidence for Late Quaternary climate change , 1994 .

[5]  P. deMenocal,et al.  Evidence for a change in the periodicity of tropical climate cycles at 2.4 Myr from whole-core magnetic susceptibility measurements , 1989, Nature.

[6]  F. Oldfield,et al.  Magnetic studies of erosion in a Scottish lake catchment. 1. Core chronology and correlation1 , 1985 .

[7]  R. Thompson,et al.  Magnetic susceptibility and particle-size distribution in Recent sediments of the Loch Lomond drainage basin, Scotland , 1979 .

[8]  F. Oldfield,et al.  Magnetic measurements used to assess sediment influx at Llyn Goddionduon , 1979, Nature.

[9]  T. Walsh,et al.  Magnetic susceptibility stratigraphy of Pacific Pleistocene sediments , 1975, Nature.

[10]  R. Thompson.  Palaeolimnology and Palaeomagnetism , 1973, Nature.

[11]  J. Lees.  Modelling the magnetic properties of natural and environmental materials , 1994 .

[12]  S. Robinson.  Applications for whole-core magnetic susceptibility measurements of deep-sea sediments: ODP Leg 115 results , 1990 .

[13]  I. Snowball,et al.  The occurrence of Greigite in sediments from Loch Lomond , 1988 .