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Order or chaos? Origin and mode of emplacement of breccias in floors of large impact structures
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“Vredefort is eroded below the original floor of the impact structure and allochthonous impact lithologies are limited to nine radial and concentric dikes of impact-melt rock, known as Vredefort Granophyre, in the crystalline core (Therriault et al. 1996a) and pseudotachylitic breccia dikes, and networks (Dressler and Reimold 2004;Reimold and Gibson 2005).”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Dressler and Reimold 2004
In the citing paper
“The additional number of motions on individual thrusts and reverse faults, spaced a few (~5-10 km) kilometers apart, apparent in industry data and the lack of specific spatial concentrations in the numbers of such structures (Fig. 3) are consistent with the observation that there are no specific spatial/radial concentrations in the development of Vredefort-related pseudotachylitic breccia exterior”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Dressler and Reimold 2004
In the citing paper
“The similar composition of pseudotachylitic breccia veins and their host rocks and the observation of relatively minor displacements (generally less than 0.5 m) across such veins at Sudbury and Vredefort would, however, seem to argue against major individual motions at smaller scales (Dressler and Reimold 2004).”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Dressler and Reimold 2004
In the citing paper
“At these levels, movement appears to have been accomplished by cumulative small-scale differential rock displacements (shearing and rotation) that is facilitated by pervasive pseudotachylitic breccia veining and high postshock temperatures (Lana et al. 2003;Dressler and Reimold 2004;Gibson and Reimold 2005).”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Dressler and Reimold 2004
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GRIEVE, R. A. F., REIMOLD, W. U., MORGAN, J., RILLER, U., & PILKINGTON, M. (2008) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2008.tb01086.x · Cited by 90
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- Authors
- Dressler, B. O., & Reimold, W. U.
- Venue
- Earth-Science Reviews
- Publisher
- Elsevier BV
- Published
- 2004-09
- Volume
- 67
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- Pages
- 1-54
- ISSN
- 0012-8252
- Cited by
- 66
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