FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2140070200> ?p ?o ?g. }

• W2140070200 endingPage "558" @default.
• W2140070200 startingPage "541" @default.
• W2140070200 abstract "We have reinvestigated the coupled thermal and crustal evolution of Mars taking new laboratory data concerning the flow behavior of iron-rich olivine into account. The low mantle viscosities associated with the relatively higher iron content of the martian mantle as well as the observed high concentrations of heat producing elements in a crust with a reduced thermal conductivity were found to promote phases of crustal recycling in many models. As crustal recycling is incompatible with an early separation of geochemical reservoirs, models were required to show no episodes of crustal recycling. Furthermore, admissible models were required to reproduce the martian crust formation history, to allow for the formation of partial melt under present day mantle conditions and to reproduce the measured concentrations of potassium and thorium on the martian surface. Taking dehydration stiffening of the mantle viscosity by the extraction of water from the mantle into account, we found that admissible models have low initial upper mantle temperatures around 1650 K, preferably a primordial crustal thickness of 30 km, and an initially wet mantle rheology. The crust formation process on Mars would then be driven by the extraction of a primordial crust after core formation, cooling the mantle to temperatures close to the peridotite solidus. According to this scenario, the second stage of global crust formation took place over a more extended period of time, waning at around 3500 Myr b.p., and was driven by heat produced by the decay of radioactive elements. Present-day volcanism would then be driven by mantle plumes originating at the core–mantle boundary under regions of locally thickened, thermally insulating crust. Water extraction from the mantle was found to be relatively efficient and close to 40% of the total inventory was lost from the mantle in most models. Assuming an initial mantle water content of 100 ppm and that 10% of the extracted water is supplied to the surface, this amount is equivalent to a 14 m thick global surface layer, suggesting that volcanic outgassing of H2O could have significantly influenced the early martian climate and increased the planet’s habitability." @default.
• W2140070200 created "2016-06-24" @default.
• W2140070200 creator A5015066564 @default.
• W2140070200 creator A5040112897 @default.
• W2140070200 creator A5044271255 @default.
• W2140070200 date "2011-04-01" @default.
• W2140070200 modified "2023-10-18" @default.
• W2140070200 title "Crustal recycling, mantle dehydration, and the thermal evolution of Mars" @default.
• W2140070200 cites W1506661083 @default.
• W2140070200 cites W1540907122 @default.
• W2140070200 cites W1544289921 @default.
• W2140070200 cites W1585654991 @default.
• W2140070200 cites W1599080806 @default.
• W2140070200 cites W1652464131 @default.
• W2140070200 cites W1660739765 @default.
• W2140070200 cites W1821593081 @default.
• W2140070200 cites W1966486780 @default.
• W2140070200 cites W1968851249 @default.
• W2140070200 cites W1969859799 @default.
• W2140070200 cites W1970929689 @default.
• W2140070200 cites W1972500665 @default.
• W2140070200 cites W1976463122 @default.
• W2140070200 cites W1977202349 @default.
• W2140070200 cites W1987269381 @default.
• W2140070200 cites W1990597914 @default.
• W2140070200 cites W1990740187 @default.
• W2140070200 cites W1990823670 @default.
• W2140070200 cites W1992383389 @default.
• W2140070200 cites W1994559944 @default.
• W2140070200 cites W1994560589 @default.
• W2140070200 cites W1999414867 @default.
• W2140070200 cites W1999460376 @default.
• W2140070200 cites W1999952187 @default.
• W2140070200 cites W2002041994 @default.
• W2140070200 cites W2007602037 @default.
• W2140070200 cites W2012434233 @default.
• W2140070200 cites W2015046051 @default.
• W2140070200 cites W2021648887 @default.
• W2140070200 cites W2027175556 @default.
• W2140070200 cites W2035651914 @default.
• W2140070200 cites W2035829575 @default.
• W2140070200 cites W2039478543 @default.
• W2140070200 cites W2040136115 @default.
• W2140070200 cites W2040744920 @default.
• W2140070200 cites W2041781155 @default.
• W2140070200 cites W2043691935 @default.
• W2140070200 cites W2044890164 @default.
• W2140070200 cites W2050756326 @default.
• W2140070200 cites W2052022937 @default.
• W2140070200 cites W2054859613 @default.
• W2140070200 cites W2056369649 @default.
• W2140070200 cites W2058490020 @default.
• W2140070200 cites W2061379388 @default.
• W2140070200 cites W2063177379 @default.
• W2140070200 cites W2063436465 @default.
• W2140070200 cites W2063830606 @default.
• W2140070200 cites W2063948740 @default.
• W2140070200 cites W2065842750 @default.
• W2140070200 cites W2066852613 @default.
• W2140070200 cites W2067892259 @default.
• W2140070200 cites W2072165703 @default.
• W2140070200 cites W2072519404 @default.
• W2140070200 cites W2073311665 @default.
• W2140070200 cites W2075542269 @default.
• W2140070200 cites W2078779540 @default.
• W2140070200 cites W2083935149 @default.
• W2140070200 cites W2085695509 @default.
• W2140070200 cites W2093295975 @default.
• W2140070200 cites W2094531287 @default.
• W2140070200 cites W2095798596 @default.
• W2140070200 cites W2096724893 @default.
• W2140070200 cites W2097784732 @default.
• W2140070200 cites W2099914884 @default.
• W2140070200 cites W2102327427 @default.
• W2140070200 cites W2110420837 @default.
• W2140070200 cites W2112503764 @default.
• W2140070200 cites W2118212541 @default.
• W2140070200 cites W2119685988 @default.
• W2140070200 cites W2120345909 @default.
• W2140070200 cites W2121781058 @default.
• W2140070200 cites W2138575508 @default.
• W2140070200 cites W2138835548 @default.
• W2140070200 cites W2140190673 @default.
• W2140070200 cites W2143855186 @default.
• W2140070200 cites W2146471836 @default.
• W2140070200 cites W2153624297 @default.
• W2140070200 cites W2155311025 @default.
• W2140070200 cites W2159045318 @default.
• W2140070200 cites W2162469299 @default.
• W2140070200 cites W2168599672 @default.
• W2140070200 cites W2171105019 @default.
• W2140070200 cites W4231989839 @default.
• W2140070200 cites W4249619451 @default.
• W2140070200 cites W4256621780 @default.
• W2140070200 doi "https://doi.org/10.1016/j.icarus.2010.12.028" @default.
• W2140070200 hasPublicationYear "2011" @default.
• W2140070200 type Work @default.
• W2140070200 sameAs 2140070200 @default.

• next