Cretaceous owing: sequencing laissez

A million-year-scale astronomical control on Late Cretaceous sea-level 3 Fig.1. Bio-, litho-, and chemostratigraphy of the studied section along with cyclostratigraphic interpretation.

Mid Cretaceous orbitolinid (Foraminiferida) record from the islands of Cres and Losinj (Croatia) and its regional stratigraphic. Owing to synsedimen-. dierentiation during the early Aptian is the sequence of strata on Losinj (Figure 4). Unlike the situation in

The belt has resulted from the closure of the Neo-Tethys Ocean owing to the convergence of the Arabian plate with Eurasia during the late Cretaceous and Cenozoic (Berberian and King, 1981, Talbot and Alavi, 1996). The study area is located in the southern foothills of the Bekhme Gorge in the Akri-Bijeel concession block .

Cretaceous Sequence W-E – 40 23. SoSo Field, Jasper and Jones Counties, Index Map and Strati graphic Section showing Lower Cretaceous Sequence N-S 40 24. Cranfield Field, Adams and Franklin Counties, Structure Map, Datum, Top of Paluxy – 40 25. Cranfield Field, Adams County, Stratigraphic Section showing Lower Cretaceous Sequence S-S’ _ 48 26.

of 0-2, owing to high accumulation rates, although this also depends on event frequencies. Upper surfaces of individual storm/river-flood beds may show BI values of 4-5, reflecting the transition to longer-lived fair-weather conditions. fair-weather waves facilitate persistent agitation near the bed, buffering environmental stresses.

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Figure 2: Stratigraphic correlation of the main fossil-bearing layers of the lower Yixian Formation.

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collapse of the Yucatan platform margin owing to ballistic ow from the chicxulub impact. introduction impact-related sedimentary deposits have been described at Cretaceous-Tertiary (K-T) boundary sites in the YucatanPen-insula region (e.g., Pope et al., 1999). In addition, coarse clastic sequences of impact origin have been reported from.

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