Age models based on palaeomagnetic measurements for the two cores analysed, CON01-603-2 (Continent Ridge) and VER98-1-14 (Academician Ridge) showing the correlation points to the reference record

Description: Palaeomagnetism was the method used for dating sediments older than the time span covered by AMS 14C dating. Geomagnetic palaeointensities recorded in Lake Baikal sediments were tuned to a reference curve (the record from ODP Site 984, Channell, 1999) whose chronology is well constrained (Demory et al., 2005a-this volume and Demory et al., 2005b-this volume). The palaeointensity record from ODP Site 984 is of high quality, is well dated and covers the time span of the present study. Anchored by a geomagnetic excursion (the Iceland basin event, dated at 186–189 ka according to Channell et al. (1997)), this age model is constrained by 55 correlation points for a time span of ca. 200 ky. The age models for both core sections in the interval 100–150 ky are shown in Fig. 2.

Global identifier:

Doi(
    "10.1594/GFZ.SDDB.1046",
)

Origins: /Wissenschaft/GFZ Data Services

Tags: Studie ? Sediment ? R/V Vereshchagin ? Vereshchagin 98 Expedition ? Vereshchagin Long Cores Expedition 2001 ? age (calendar years) ? correlation of paleointensity records ?

License: unbekannt

Language: Englisch/English

Organisations

• Deutsches GeoForschungsZentrum GFZ (Herausgeberschaft)

Issued: 2006-01-01

Time ranges: 2006-01-01 - 2006-01-01

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Aktiv

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