Arabia Terra, Mars: Tectonic and Palaeoclimatic Evolution of a Remarkable Sector of Martian Lithosphere

@article{Anguita1997ArabiaTM,
  title={Arabia Terra, Mars: Tectonic and Palaeoclimatic Evolution of a Remarkable Sector of Martian Lithosphere},
  author={Francisco Anguita and Jorge Anguita and Gabriel Castilla and M.{\'A}. De la Casa and J. Dom{\'i}nguez and Raquel Herrera and Pilar Llanes and M{\'o}nica Guti{\'e}rrez L{\'o}pez and Vicente Carlos Ruiz Mart{\'i}nez},
  journal={Earth, Moon, and Planets},
  year={1997},
  volume={77},
  pages={55-72}
}
A regional geologic study of Arabia Terra, a densely cratered area of Mars northern hemisphere, has revealed the individuality of this province. This is best expressed by an equatorial belt with a crater age distinctly younger as compared to the northern part of Arabia Terra and to Noachis Terra to the south. We interpret this as an incipient back-arc system provoked by the subduction of Mars lowlands under Arabia Terra during Noachian times. The regional fracture patterns are also best… 
Evidence of Regionally Distributed Tectono‐Volcanism in a Floor Fractured Crater of North‐Central Arabia Terra, Mars
Arabia Terra features many tectonic structures, which have been correlated to episodes of incipient tectonics, massive impacts, and controls on fluvial systems. However, the extent of regionally
Generic identification and classification of morphostructures in the Noachis-Sabaea region, southern highlands of Mars
ABSTRACT The Noachis-Sabaea region in the southern highlands preserves some of the oldest Martian crust. It records deformation by both endogenic and exogenic processes. This deformation includes
Crustal history of north central Arabia Terra, Mars
Detailed geological studies across the highland-lowland boundary in north central Arabia Terra, Mars provide constraints on the age and nature of processes responsible for a complex array of
An Introduction to its Interior, Surface and Atmosphere
Page 115, equation 5.11: The transient crater depth (dt) is 1/10 of the transient diameter (Dt), thus equation 5.11 should read: 1 30 Page 118, equation 5.12: Should be Dt, not D. Page 163, last
Identifying Evidence for Explosive Volcanism on Mars Through Geomorphologic and Thermophysical Observations
...................................................................................................................... vi LIST OF TABLES
Formation and erosion of layered materials: Geologic and dust cycle history of eastern Arabia Terra, Mars
[1] Eastern Arabia Terra is mantled in a layer of dust a few centimeters to a meter thick, yet contains morphologic features that suggest a history of multiple events of deposition and consolidation
Mars: An Introduction to its Interior, Surface and Atmosphere: References
Our knowledge of Mars has changed dramatically in the past 40 years due to the wealth of information provided by Earth-based and orbiting telescopes, and spacecraft investigations. Recent

References

SHOWING 1-10 OF 67 REFERENCES
Mottled terrain: a continuing Martian enigma.
The mottled plains material found in the northern Martian lowlands is discussed in terms of Mariner and Viking images as well as geologic mapping based on Viking images. The mottling in Mariner 9
Is the Gordii Dorsum escarpment on Mars an exhumed transcurrent fault?
Investigators of deformation features on the surface of Mars have generally concluded that fault zones with major horizontal displacements do not occur or have not been preserved1–5. Here we present
Geochemical evolution of the northern Plains of Mars: early hydrosphere, carbonate development, and present morphology.
It is likely that early in Mars' history, abundant liquid water was available. Under a thick (several bars) carbon dioxide atmosphere, this water could have formed an ocean, located primarily in the
Coastal Geomorphology of the Martian northern plains
The paper considers the question of the formation of the outflow channels and valley networks discovered on the Martian northern plains during the Mariner 9 mission. Parker and Saunders (1987) and
Chronology and global distribution of fault and ridge systems on Mars
Paleotectonic maps are presented showing fault and ridge systems on Mars as they existed during successive geologic periods: the Noachian, Hesperian, and Amazonian Periods, and their eight epoch
Tectonic evolution of Mars
Any model for the tectonic evolution of Mars must account for two major crustal elements: the Tharsis bulge and the topographically low and lightly cratered northern third of the planet. Ages
System of tectonic features common to Earth, Mars, and Venus
Investigations of landforms on the terrestrial planets have revealed a system of tectonic features consisting of long, narrow, regularly spaced folds and/or thrust faults, referred to as wrinkle
Age relations of Martian highland drainage basins
Dendritic valley patterns in the equatorial highlands of Mars show evidence of internal drainage into restricted basins, which are interpreted to be floored with sedimentary fill. Based on crater
Martian permafrost features
The outgassing history of Mars and the prevailing temperature conditions suggest that ground ice may occur to depths of kilometers over large areas of the planet. The presence of permafrost is also
...
...