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https://doi.org/10.1130/0091-7613(2002)030<0091:ccitbc>2.0.co;2
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Cite Journal: Geology |  Publication Date: Jan 1, 2002 |
 Citations: 4 |
Affiliation: Universidad de Zaragoza, Centro de Astrobiología
[Ernstson et al. (2001)][1] interpreted pitted and fractured quartzite cobbles of Lower Triassic conglomerates as new evidence in support of the existence of two large impact structures in the Iberian chain: Azuara and Rubielos de la Cerida ([Fig. 1][2]). In this discussion we disagree with their
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