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Lithospheric Dynamics of Mars - Water, Flow, and Failure (Paperback)
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Lithospheric Dynamics of Mars - Water, Flow, and Failure (Paperback)
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Some of the largest Martian erosive features were influenced by
groundwater, and include valley networks, outflow channels, and
possibly landslides. We argue that hydrothermal systems attending
crustal formation processes were able to drive sufficient
groundwater to the surface to form the Noachian southern highlands
valley networks, which show a spatial correlation to crustal
magnetic anomalies, also results of crustal formation. Hydrothermal
activity is quantified through numerical simulations of convection
in a porous medium due to the presence of a hot intruded magma
chamber. The parameter space includes magma chamber depth, volume,
aspect ratio, and host rock permeability and porosity. For
permeabilities as low as l0(exp -17) sq m and intrusion volumes as
low as 50 km, the total discharge due to intrusions building that
part of the southern highlands crust associated with magnetic
anomalies spans a comparable range as the inferred discharge from
the overlying valley networks. The Hesperian circum-Chryse outflow
channels are further manifestations of groundwater discharge and
Clifford and Parker (2001) suggest that the large volumes of water
required for their formation flows beneath a confining cryosphere
from the South Pole where meltwater beneath an ice cap recharges a
global aquifer. We argue that recharge occurs instead over the
nearby Tharsis aquifer at high obliquity, assisted by cryosphere
melting due to volcanic activity. Numerical simulations quantify
the strength and duration of outflow discharge given either South
Polar or Tharsis recharge. The contribution of South Pole recharge
given Clifford and Parker aquifer properties is negligible compared
to that of the initial Tharsis inventory. Tharsis recharge, despite
the restrictions of improved aquifer properties, makes a
significant contribution and, unlike South Pole recharge under the
same conditions, fulfills discharge requirements.
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