Palaeoenvironments and weathering regime of the Neoproterozoic Squantum ‘Tillite’, Boston Basin: no evidence of a snowball Earth-Reference-Cited by-同舟云学术

Palaeoenvironments and weathering regime of the Neoproterozoic Squantum ‘Tillite’, Boston Basin: no evidence of a snowball Earth

Published:2010-09-14 Issue:6 Volume:57 Page:1526-1544
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:

Author:

PASSCHIER SANDRA,ERUKANURE EFE

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-3091.2010.01154.x/fullpdf

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3. Quartz sand surface textural evidence for a glacial origin of the Squantum “Tillite”, Boston Basin, Massachusetts: comments and reply;Baker;Geology,1975

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5. Geochronological constraints on terminal Neoproterozoic events and the rise of metazoans;Bowring;Geophys. Res. Abstr.,2003

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