Titlebook: Chronology and Evolution of Mars; Proceedings of an IS Reinald Kallenbach,Johannes Geiss,William K. Hartm Conference proceedings 2001 Sprin

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Einführung in die digitale Regelunged to terrestrial basalts and eucrites may be related to this higher phosphorus content. The highly siderophile element abundance patterns have been interpreted as reflecting strong partitioning during core formation in a magma ocean environment with little if any late veneer. Oxygen isotope data pr

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Einführung in die Mehrgrößenregelungickness can be shown to be in agreement with estimates of volcanic production rates from geologic mapping using data from the camera on MGS and previous missions. According to these estimates most of the crust was produced in the Noachian, roughly the first Gyr of evolution. A substantial part of th

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Conference proceedings 2001 cessation of major collisional growth on Mars. Finally, we reevaluate the isotopic evidence that Mars differentiated quickly. Fundamental differences between the composition of Mars and that of other terrestrial planets are apparent from the planet‘s slightly lower density and from the compositions

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