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  • 1
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    In:  Rev. Geophys. Space Phys., Luxembourg, National Academy of Sciences of the USA, vol. 17, no. 6, pp. 981-1019, pp. B05311, (ISSN: 1340-4202)
    Publication Date: 1979
    Keywords: Stress ; Plate tectonics ; Review article ; Tectonics
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  • 2
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    In:  J. Geophys. Res., Warszawa, Polish Geothermal Association, vol. 84, no. 7, pp. 1667-1682, pp. B05406, (ISSN: 1340-4202)
    Publication Date: 1979
    Keywords: Stress ; Elasticity ; Planetology ; Tectonics ; JGR
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  • 3
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    In:  J. Geophys. Res., Warszawa, Conseil de l'Europe, vol. 81, no. 2, pp. 921-930, pp. L19608, (ISBN: 0-12-018847-3)
    Publication Date: 1976
    Keywords: Plate tectonics ; JGR
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  • 4
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    In:  Pageoph, Luxembourg, National Academy of Sciences of the USA, vol. 115, no. 6, pp. 317-332, pp. B05311, (ISSN: 1340-4202)
    Publication Date: 1977
    Keywords: Seismology ; Stress ; Stress drop ; Tectonics
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  • 5
    Publication Date: 1979-09-14
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Coleman, P J Jr -- Fuller, M -- Housley, R M -- Latham, G V -- Runcorn, S K -- Sjogren, W J -- Solomon, S C -- Sonett, C P -- New York, N.Y. -- Science. 1979 Sep 14;205(4411):1082-3.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17735028" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2019-06-27
    Description: The relationship between crustal tectonics and thermal evolution is discussed in terms of the moon and Mercury. Finite strain theory and depth and temperature-dependent thermal expansion are used to evaluate previous conclusions about early lunar history. Factors bringing about core differentiation in the first 0.6 b.y. of Mercurian evolution are described. The influence of concentrating radioactive heat sources located in Mercury's crust on the predicted contraction is outlined. The predicted planetary volume change is explored with regard to quantitative limits on the extent of Mercurian core solidification. Lunar and Mercurian thermal stresses involved in thermal evolution are reviewed, noting the history of surface volcanism. It is concluded that surface faulting and volcanism are closely associated with the thermal evolution of the whole planetary volume. As the planet cools or is heated, several types of tectonic and volcanic effects may be produced by thermal stress occurring in the lithosphere.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Format: text
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  • 7
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    In:  Other Sources
    Publication Date: 2019-06-27
    Description: Some questions dealing with the nature and history of a large metallic core within Mercury are considered. These include the existence of a core, its size, whether it is fluid or solid, the timescale for core formation, the geological consequences of core formation, and whether such consequences are consistent with the surface geology. Several indirect lines of evidence are discussed which suggest the presence of a large iron-rich core. A core-formation model is examined in which core infall is accompanied by an increase of 17 km in planetary radius, an increase of 700 K in mean internal temperature, and substantial melting of the mantle. It is argued that if the core differentiated from an originally homogeneous planet, that event must have predated the oldest geological units comprising most of the planetary surface. A convective dynamo model for the source of Mercury's magnetic field is shown to conflict with cosmochemical models that do not predict a substantial radiogenic heat source in the core.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Icarus; 28; Aug. 197
    Format: text
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  • 8
    Publication Date: 2019-07-13
    Description: The thickness (T) of the lunar elastic lithosphere at the time (3.6 to 3.8 billion years ago) of the earliest preserved basalt flows in circular mare basins can be estimated by inverting the observed locations of extensional tectonic features in and surrounding the maria. In performing the inversion, the lithosphere is modeled as an elastic shell with a liquid interior, and the basalt load for each mare is approximated by a set of concentric cylinders. To permit solving the forward problem of placing radial limits on the positions of the rilles around a given mare, an additional parameter F, the ratio of the radial stress at the radial limits to the maximum radial stress, is introduced. T and F are chosen to give the best weighted-squares fit of the radial limits to the observations, and are used as the initial values in a linearized matrix inversion to check the resolution and estimate errors. The application of the procedure to three maria with prominent extensional features, Humorum, Orientale, and Serenitatis, gives values of T from about 40 + or - 10 to 50 + or - 10 km, and in each case the linearized matrix equation has an exact inverse.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Lunar and Planetary Science Conference; Mar 19, 1979 - Mar 23, 1979; Houston, TX
    Format: text
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  • 9
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    In:  Other Sources
    Publication Date: 2019-07-13
    Description: It is pointed out that the concept of hydrostatic head, the height to which a fluid at a given pressure will rise in a gravitational field, can be usefully applied to magmatic liquids and to a number of problems in volcanology. For the moon, hydrostatic head arguments are an essential ingredient to explanations of mascons and of the scarcity of farside maria. In the reported investigation, simple hydrostatic concepts are extended to synthesize results from experimental petrology, lunar chronology, thermal history models, seismology, and gravity. Attention is given to a scenario for early lunar history, the density of lunar rocks and basaltic liquids, the thickness of the lunar crust, the source depth of mare basalt versus time, hydrostatic considerations with respect to the occurrence of high-titanium and low-titanium mare basalts, the structure of mascons, and the extension of the concepts of hydrostatics to the parent liquids of other basaltic rocks returned from the lunar surface.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Lunar Science Conference; Mar 17, 1975 - Mar 21, 1975; Houston, TX
    Format: text
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  • 10
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    In:  CASI
    Publication Date: 2019-07-13
    Description: An evaluation of existing theories on the existence of the planet's metallic core is presented. Topics considered are: (1) magnetic fields; (2) surface geology; (3) cosmochemical models.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: NASA-CR-143322 , Intern. Colloq. on Mercury; Jun 01, 1975
    Format: application/pdf
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