What is the average thickness of continental crust




















Chemi Geol 3—4 — Geochem Geophys Geosyst 14 6 — Science — CrossRef Google Scholar. Jagoutz O, Schmidt MW The composition of the foundered complement to the continental crust and a re-evaluation of fluxes in arcs.

Elsevier, Oxford, pp 53—72 Google Scholar. Earth-Sci Rev — Kamber BS Archean mafic-ultramafic volcanic landmasses and their effect on ocean atmosphere chemistry. Chem Geol 1—2 — Geochim Cosmochim Acta 69 4 — Kelemen PB Genesis of high Mg andesites and the continental crust. Nat Geosci — Kelemen PB et al a Along-strike variation in lavas of the Aleutian island arc: implications for the genesis of high Mg andesite and the continental crust.

Kelemen PB, Hanghoj K, Greene A b One view of the geochemistry of subduction-related magmatic arcs, with an emphasis on primitive andesite and lower crust. Elsevier, Amsterdam, pp — Google Scholar. Keller CB, Schoene B Statistical geochemistry reveals disruption in secular lithospheric evolution about 2. In: Rudnick RL ed The crust, vol 4. Earth Planet Sci Lett 1—2 — Precambrian Res — Geology 44 6 — Nat Geosci 3 9 — Geochim Cosmochim Acta 75 8 — Lee CTA Physics and chemistry of deep continental crust recycling.

Insights from Zr and P systematics. Nat Geosci 9 6 — Li S, Gaschnig RM, Rudnick RL Insights into chemical weathering of the upper continental crust from the geochemistry of ancient glacial diamictites. Liu X-M, Rudnick RL Constraints on continental crustal mass loss via chemical weathering using lithium and its isotopes. Narryer and Jack Hills, Western Australia. Geochimica Et Cosmochimica Acta 56 3 — Martin H Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas.

Martin H, Moyen JF Secular changes in tonalite-trondhjemite-granodiorite composition as markers of the progressive cooling of Earth. Geology 30 4 — CrossRef Google Scholar. McLennan SM Relationships between the trace element composition of sedimentary rocks and upper continental crust. Geochem Geophys Geosyst 2:art. Chem Geol 3—4 — Australian post-Archean sedimentary-rocks. Geochim Cosmochim Acta 40 12 — Archean sedimentary-rocks from Kalgoorlie, Australia. Geochim Cosmochim Acta 41 2 — Precambrian Res 78 1—3 :1— Parman SW Time-lapse zirconography: imaging punctuated continental evolution.

Geochem Perspect Lett — J Geophys ResSolid Earth 3 — Peucker-Ehrenbrink B, Jahn B-M Rhenium-osmium isotope systematics and platinum group element concentations: loess and the upper continental crust. Nat Geosci. Reubi O, Blundy J A dearth of intermediate melts at subduction zone volcanoes and the petrogenesis of arc andesites. Nature —U Rollinson H Secular evolution of the continental crust: implications for crust evolution models. Geochem Geophys Geosyst 9. Geochem Geophys Geosyst 15 6 — Rudnick RL Making continental crust.

In: Rudnick RL ed The crust, vol 3. Elsevier, Amsterdam, pp 1—64 Google Scholar. Elements 3 1 — Schoene B U-Pb geochronology. Simon L, Lecuyer C Continental recycling: the oxygen isotope point of view. Geochem Geophys Geosyst 6:Q Nature —68 CrossRef Google Scholar. Geology 43 8 — Taylor SR Abundance of chemical elements in the continental crust — a new table. Taylor SR Island arc models and the composition of the continental crust. Blackwell, Oxford Google Scholar. Geochem Geophys Geosyst 1.

Depth-dependent flux of H2O from subducting slabs worldwide. J Geophys ResSolid Earth Geochim Cosmochim Acta 40 8 — Voice PJ, Kowalewski M, Eriksson KA Quantifying the timing and rate of crustal evolution: global compilation of radiometrically dated detrital zircon grains.

J Geol 2 — Wedepohl H The composition of the continental crust. Yanagi T, Yamashita K Genesis of continental-crust under island-arc conditions.

Lithos 33 1—3 — Roberta L. Rudnick 1 2 Email author 1. All three major rock types—igneous, metamorphic, and sedimentary—are found in the crust. Continental crust is less dense because of its composition. Continental crust is made up of felsic material SiO4 — mainly granite.

The density of continental crust is 2. Oceanic crust, while thinner, is made of mafic materials Fe, Mg — mainly basalt. The average density of oceanic crust is 3. The plate is either of general polygonal shape or of circular shape. Unlike the mineral-rich crust and mantle, the core is made almost entirely of metal—specifically, iron and nickel. Elements that dissolve in iron, called siderophiles, are also found in the core.

The core is thought to be so hot due to the decay of radioactive elements, leftover heat from planetary formation, and heat released as the liquid outer core solidifies near its boundary with the inner core. This means rocks, topsoil, trees, buildings, your pet dog, and so on, would be swept away into the atmosphere.

The solid inner core turns only once every years or so, relative to the rest of the planet. No one knows the real reason for field reversals. Skip to content Natural sciences. What is the approximate thickness of a continental crust?



0コメント

  • 1000 / 1000