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Gravity surveys of impact structures Gravity anomalies in impact structures may result from quite different processes. Small, simple craters in general show a roughly circular negative anomaly (e.g., Fig. 11). A low-density breccia lens at the crater floor, post-impact young crater sediments, and fracturing of the rocks beneath and around the crater may contribute to … Continue reading "Gravity surveys"
PDF) ERNSTSON CLAUDIN IMPACT STRUCTURES – METEORITE CRATERS
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Нердлінгер-Рис — Вікіпедія
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