Recognizable primary volcanic and sedimentary features in a low‐strain domain of the highly deformed, oldest known (≈ 3.7–3.8 Gyr) Greenstone Belt, Isua, West Greenland-Reference-Cited by-同舟云学术

Recognizable primary volcanic and sedimentary features in a low‐strain domain of the highly deformed, oldest known (≈ 3.7–3.8 Gyr) Greenstone Belt, Isua, West Greenland

Published:1998-03 Issue:2 Volume:10 Page:57-62
ISSN:0954-4879
Container-title:Terra Nova
language:en
Short-container-title:Terra Nova

Author:

Appel ¹,Fedo ²,Moorbath ³,Myers ⁴

Affiliation:

1. Geological Survey of Denmark and Greenland, 2400‐Copenhagen, Denmark.

2. Department of Geology, George Washington University, Washington, D.C. 20052, USA.

3. Department of Earth Sciences, Oxford University, Oxford OX1 3PR, UK.

4. Geological Survey of Western Australia, Perth, Western Australia.

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.1998.00162.x

Reference14 articles.

1. AllaartJ.H.1976.The pre‐3760 my. old supracrustal rocks of the Isua area central West Greenland and the associated occurrence of quartz‐banded ironstone.In:The Early History of the Earth(B.F. Windley ed.) pp.177189.Wiley London.

2. Field work on the very early Precambrian rocks of the Isua area, southern West Greenland.;Bridgwater D.;Grøn. Geol. Unders. Rep.,1973

3. DimrothE.1982.The oldest rocks on Earth: stratigraphy and sedimentology of the 3.8 billion years old Isua supracrustal sequence.In:Sedimentary Geology of the Highly Metamorphosed Precambrian Complexes(A.V. Sidorenko ed.) pp.1627.Nauka Moskow.

4. Sedimentology of archean greenstone belts: Signatures of tectonic evolution

5. Extreme Nd-isotope heterogeneity in the early Archaean—fact or fiction? Case histories from northern Canada and West Greenland—Reply

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