Experimental pictures of deformation patterns in a possible model of the Earth's interior

Ruud Weijermars

doi:10.1016/0012-821X(89)90010-1

Experimental pictures of deformation patterns in a possible model of the Earth's interior

Ruud Weijermars^*

^*Corresponding author for this work

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

8 Scopus citations

Abstract

Geophysical calculations and observations of the Earth's properties have previously established that the motion of tectonic plates and associated geological hazards are driven by extensive rock displacement in the mantle of our planet. The progressive deformation of mantle rock by solid-state convection, so far only studied in two-dimensional numerical computer simulations, can now also be studied three-dimensionally in a real fluid. Two billion years of structural developments in the Earth's upper mantle can be visualized within one hour of flow in the laboratory, assuming one particular mode of (upper) mantle circulation.

Original language	English
Pages (from-to)	367-373
Number of pages	7
Journal	Earth and Planetary Science Letters
Volume	91
Issue number	3-4
DOIs	https://doi.org/10.1016/0012-821X(89)90010-1
State	Published - Jan 1989
Externally published	Yes

Bibliographical note

Funding Information:
I sincerely thank U. Christensen, S. Cruden, H. Ramberg, H. Schmeling, C.J. Talbot, and D. Turcotte for useful comments and K. Gloersen, E. Meland and H. Harryson for technical assistance. All preliminary and final experiments, photographs, analyses and draftwork were made by the author. This study has been funded by the Swedish Natural Science Research Council (NFR).

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ASJC Scopus subject areas

Geophysics
Geochemistry and Petrology
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)

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10.1016/0012-821X(89)90010-1

Cite this

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title = "Experimental pictures of deformation patterns in a possible model of the Earth's interior",

abstract = "Geophysical calculations and observations of the Earth's properties have previously established that the motion of tectonic plates and associated geological hazards are driven by extensive rock displacement in the mantle of our planet. The progressive deformation of mantle rock by solid-state convection, so far only studied in two-dimensional numerical computer simulations, can now also be studied three-dimensionally in a real fluid. Two billion years of structural developments in the Earth's upper mantle can be visualized within one hour of flow in the laboratory, assuming one particular mode of (upper) mantle circulation.",

author = "Ruud Weijermars",

note = "Funding Information: I sincerely thank U. Christensen, S. Cruden, H. Ramberg, H. Schmeling, C.J. Talbot, and D. Turcotte for useful comments and K. Gloersen, E. Meland and H. Harryson for technical assistance. All preliminary and final experiments, photographs, analyses and draftwork were made by the author. This study has been funded by the Swedish Natural Science Research Council (NFR).",

year = "1989",

month = jan,

doi = "10.1016/0012-821X(89)90010-1",

language = "English",

volume = "91",

pages = "367--373",

journal = "Earth and Planetary Science Letters",

issn = "0012-821X",

publisher = "Elsevier B.V.",

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AU - Weijermars, Ruud

N1 - Funding Information: I sincerely thank U. Christensen, S. Cruden, H. Ramberg, H. Schmeling, C.J. Talbot, and D. Turcotte for useful comments and K. Gloersen, E. Meland and H. Harryson for technical assistance. All preliminary and final experiments, photographs, analyses and draftwork were made by the author. This study has been funded by the Swedish Natural Science Research Council (NFR).

PY - 1989/1

Y1 - 1989/1

N2 - Geophysical calculations and observations of the Earth's properties have previously established that the motion of tectonic plates and associated geological hazards are driven by extensive rock displacement in the mantle of our planet. The progressive deformation of mantle rock by solid-state convection, so far only studied in two-dimensional numerical computer simulations, can now also be studied three-dimensionally in a real fluid. Two billion years of structural developments in the Earth's upper mantle can be visualized within one hour of flow in the laboratory, assuming one particular mode of (upper) mantle circulation.

AB - Geophysical calculations and observations of the Earth's properties have previously established that the motion of tectonic plates and associated geological hazards are driven by extensive rock displacement in the mantle of our planet. The progressive deformation of mantle rock by solid-state convection, so far only studied in two-dimensional numerical computer simulations, can now also be studied three-dimensionally in a real fluid. Two billion years of structural developments in the Earth's upper mantle can be visualized within one hour of flow in the laboratory, assuming one particular mode of (upper) mantle circulation.

UR - https://www.scopus.com/pages/publications/0024525766

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DO - 10.1016/0012-821X(89)90010-1

M3 - Article

AN - SCOPUS:0024525766

SN - 0012-821X

VL - 91

SP - 367

EP - 373

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

IS - 3-4

ER -

Experimental pictures of deformation patterns in a possible model of the Earth's interior

Abstract

Bibliographical note

UN SDGs

ASJC Scopus subject areas

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