Metal veins in the Kernouvé (H6 S1) chondrite: Evidence for pre- or syn-metamorphic shear deformation

Kernouvé is an H6 chondrite that experienced a very small degree of late stage shock loading (S1). However, Kernouvé contains Fe–Ni metal vein-like structures, whose formation have been attributed to an early impact event. To establish the formation conditions of metal veins in Kernouvé, we examined...

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Veröffentlicht in:	Geochim. Cosmochim. Acta 2013-09, Vol.116 (9, 2013), p.71-83
Hauptverfasser:	Friedrich, Jon M., Ruzicka, Alex, Rivers, Mark L., Ebel, Denton S., Thostenson, James O., Rudolph, Rebecca A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Chondrites cracking deformation Grains Metamorphic micro-computed tomography microscopy Orientation Porosity Shear deformation temperature Three dimensional Veins
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