Early timing of remanence in haematite of the Neoproterozoic Elatina formation, Adelaide geosyncline: confirmation of the low palaeolatitude of Neoproterozoic glaciation

Phillip W. Schmidt; Brian J J Embleton; George E. Williams

doi:10.1071/EG993239

Early timing of remanence in haematite of the Neoproterozoic Elatina formation, Adelaide geosyncline: confirmation of the low palaeolatitude of Neoproterozoic glaciation

Phillip W. Schmidt, Brian J J Embleton^*, George E. Williams

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

9 Citations (Scopus)

Abstract

We discuss the evidence for frigid, strongly seasonal climates near sea level which preferentially existed in low palaeolatitudes during the Neoproterozoic. The Neoproterozoic glacialperiglacial palaeoclimate is one of the major paradoxes in contemporary earth science.

Original language	English
Pages (from-to)	239-242
Number of pages	4
Journal	Exploration Geophysics
Volume	24
Issue number	2
DOIs	https://doi.org/10.1071/EG993239
Publication status	Published - 1993

Keywords

Glaciation
Palaeo-climate
Palaeomagnetism
Proterozoic

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10.1071/EG993239

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title = "Early timing of remanence in haematite of the Neoproterozoic Elatina formation, Adelaide geosyncline: confirmation of the low palaeolatitude of Neoproterozoic glaciation",

abstract = "We discuss the evidence for frigid, strongly seasonal climates near sea level which preferentially existed in low palaeolatitudes during the Neoproterozoic. The Neoproterozoic glacialperiglacial palaeoclimate is one of the major paradoxes in contemporary earth science.",

keywords = "Glaciation, Palaeo-climate, Palaeomagnetism, Proterozoic",

author = "Schmidt, \{Phillip W.\} and Embleton, \{Brian J J\} and Williams, \{George E.\}",

year = "1993",

doi = "10.1071/EG993239",

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pages = "239--242",

journal = "Exploration Geophysics",

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T2 - confirmation of the low palaeolatitude of Neoproterozoic glaciation

AU - Schmidt, Phillip W.

AU - Embleton, Brian J J

AU - Williams, George E.

PY - 1993

Y1 - 1993

N2 - We discuss the evidence for frigid, strongly seasonal climates near sea level which preferentially existed in low palaeolatitudes during the Neoproterozoic. The Neoproterozoic glacialperiglacial palaeoclimate is one of the major paradoxes in contemporary earth science.

AB - We discuss the evidence for frigid, strongly seasonal climates near sea level which preferentially existed in low palaeolatitudes during the Neoproterozoic. The Neoproterozoic glacialperiglacial palaeoclimate is one of the major paradoxes in contemporary earth science.

KW - Glaciation

KW - Palaeo-climate

KW - Palaeomagnetism

KW - Proterozoic

UR - https://www.scopus.com/pages/publications/85009354455

U2 - 10.1071/EG993239

DO - 10.1071/EG993239

M3 - Article

AN - SCOPUS:85009354455

SN - 0812-3985

VL - 24

SP - 239

EP - 242

JO - Exploration Geophysics

JF - Exploration Geophysics

IS - 2

ER -

Early timing of remanence in haematite of the Neoproterozoic Elatina formation, Adelaide geosyncline: confirmation of the low palaeolatitude of Neoproterozoic glaciation

Abstract

Keywords

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