TY - JOUR
T1 - The geology of the Kerwan quadrangle of dwarf planet Ceres
T2 - Investigating Ceres’ oldest, largest impact basin
AU - Williams, David
AU - Kneissl, T.
AU - Neesemann, A.
AU - Mest, S. C.
AU - Palomba, E.
AU - Platz, T.
AU - Nathues, A.
AU - Longobardo, A.
AU - Scully, J. E.C.
AU - Ermakov, A.
AU - Jaumann, R.
AU - Buczkowski, D. L.
AU - Schäfer, M.
AU - Thangjam, G.
AU - Pieters, C. M.
AU - Roatsch, T.
AU - Preusker, F.
AU - Marchi, S.
AU - Schmedemann, N.
AU - Hiesinger, H.
AU - Frigeri, A.
AU - Raymond, C. A.
AU - Russell, C. T.
N1 - Funding Information:
The authors thank David Crown and Tracy Gregg, and editor Michael Bland for productive and helpful reviews. The authors also thank the NASA Dawn Science and Flight Teams at the Jet Propulsion Laboratory for their tireless work that enabled the successful Ceres mission, and the instrument teams at the Max Planck Institute for Solar System Research, the German Aerospace Center (DLR), the Italian National Institute of Astrophysics (INAF), and the Planetary Science Institute for collecting and processing the data that enabled this study. The funding for this research was provided under NASA contract NNM05AA86 through a subcontract from the University of California, Los Angeles. The VIR Team is funded by the Italian Space Agency (ASI) through grant number I/004/12/0 . We acknowledge the support of the Ronald Greeley Center for Planetary Studies, the NASA Regional Planetary Information Facility (RPIF) at ASU, without which this research could not have been done.
Funding Information:
The authors thank David Crown and Tracy Gregg, and editor Michael Bland for productive and helpful reviews. The authors also thank the NASA Dawn Science and Flight Teams at the Jet Propulsion Laboratory for their tireless work that enabled the successful Ceres mission, and the instrument teams at the Max Planck Institute for Solar System Research, the German Aerospace Center (DLR), the Italian National Institute of Astrophysics (INAF), and the Planetary Science Institute for collecting and processing the data that enabled this study. The funding for this research was provided under NASA contract NNM05AA86 through a subcontract from the University of California, Los Angeles. The VIR Team is funded by the Italian Space Agency (ASI) through grant number I/004/12/0. We acknowledge the support of the Ronald Greeley Center for Planetary Studies, the NASA Regional Planetary Information Facility (RPIF) at ASU, without which this research could not have been done.
Publisher Copyright:
© 2017 Elsevier Inc.
PY - 2018/12
Y1 - 2018/12
N2 - We conducted a geologic mapping investigation of Dawn spacecraft data to determine the geologic history of the Kerwan impact basin region of dwarf planet Ceres, which is mostly located in the Ac-7 Kerwan Quadrangle. Geological mapping was applied to Dawn Framing Camera images from the Low Altitude Mapping Orbit (LAMO, 35 m/pixel) and supplemented by digital terrain models and color images from the High Altitude Mapping Orbit (HAMO, 135 m/pixel), as well as preliminary Visible and Infrared Spectrometer (VIR) and gravity data. The 284-km diameter Kerwan impact basin is the oldest unequivocal impact crater on Ceres, and has a highly discontinuous, polygonal, degraded rim and contains a 'smooth’ unit that both fills the basin floor and surrounds the degraded rim to the west, south, and east. Although there are some subtle topographic features in the Kerwan basin that could be interpreted as flow boundaries, there is no indisputable evidence of cryovolcanic features in or around the basin (however if such features existed they could be buried). Nevertheless, all data point to impact-induced melting of a cerean crust enriched in a volatile, likely water ice, to produce the Kerwan smooth material. Subsequent geologic activity in this region includes emplacement of impact craters such as Dantu, which produced a variety of colorful deposits, and rayed craters such as Rao and Cacaguat. Based on the crater size-frequency distribution absolute model ages of the Kerwan smooth material in and around the basin, marking a minimum age for the Kerwan basin, our mapping defines this as the oldest boundary within the cerean geologic timescale, separating the Pre-Kerwanan and Kerwanan Periods at > 1.3 Ga (Lunar-derived chronology model) or > 230–850 Ma (Asteroid-derived chronology model, depending on strength of target material).
AB - We conducted a geologic mapping investigation of Dawn spacecraft data to determine the geologic history of the Kerwan impact basin region of dwarf planet Ceres, which is mostly located in the Ac-7 Kerwan Quadrangle. Geological mapping was applied to Dawn Framing Camera images from the Low Altitude Mapping Orbit (LAMO, 35 m/pixel) and supplemented by digital terrain models and color images from the High Altitude Mapping Orbit (HAMO, 135 m/pixel), as well as preliminary Visible and Infrared Spectrometer (VIR) and gravity data. The 284-km diameter Kerwan impact basin is the oldest unequivocal impact crater on Ceres, and has a highly discontinuous, polygonal, degraded rim and contains a 'smooth’ unit that both fills the basin floor and surrounds the degraded rim to the west, south, and east. Although there are some subtle topographic features in the Kerwan basin that could be interpreted as flow boundaries, there is no indisputable evidence of cryovolcanic features in or around the basin (however if such features existed they could be buried). Nevertheless, all data point to impact-induced melting of a cerean crust enriched in a volatile, likely water ice, to produce the Kerwan smooth material. Subsequent geologic activity in this region includes emplacement of impact craters such as Dantu, which produced a variety of colorful deposits, and rayed craters such as Rao and Cacaguat. Based on the crater size-frequency distribution absolute model ages of the Kerwan smooth material in and around the basin, marking a minimum age for the Kerwan basin, our mapping defines this as the oldest boundary within the cerean geologic timescale, separating the Pre-Kerwanan and Kerwanan Periods at > 1.3 Ga (Lunar-derived chronology model) or > 230–850 Ma (Asteroid-derived chronology model, depending on strength of target material).
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U2 - 10.1016/j.icarus.2017.08.015
DO - 10.1016/j.icarus.2017.08.015
M3 - Article
AN - SCOPUS:85028470182
SN - 0019-1035
VL - 316
SP - 99
EP - 113
JO - Icarus
JF - Icarus
ER -