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Characteristics of marls: (a) and (b) bioturbation within calcareous marls (lens as scale in a), C org rich shale (16 wt.%) in (c) thin section and (d) outcrop.

Characteristics of marls: (a) and (b) bioturbation within calcareous marls (lens as scale in a), C org rich shale (16 wt.%) in (c) thin section and (d) outcrop.

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In fractured reservoirs characterized by low matrix permeability, fracture networks control the main fluid flow paths. However, in layered reservoirs, the vertical extension of fractures is often restricted to single layers. In this study, we explored the effect of changing marl/shale thickness on fracture extension using comprehensive field data a...

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Context 1
... laminae observed in the field or thin sections (Fig. 4b,d). CaCO 3 content of CMs and LCMs ranges from 44 wt.% to 82 wt.%; both are slightly higher than the content of RMs and LMs (25e56 wt.%) ( Table 1). Within some marls, sharply defined color changes, from light grey to dark grey, occur along strongly bioturbated transitions (Chondrites type; Fig. 5a and b). Thin sections reveal that these Table 1 Lithology, average bed thickness (cm), CaCO 3 and C org content (wt.%) of each bed collected in all sections. WBL ¼ well-bedded limestones, SNL ¼ semi-nodular limestones, CM ¼ calcareous marls, LCM ¼ laminated calcareous marls, LM ¼ laminated marls, RM ¼ regular marls. Please note that all ...
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... tubes are ubiquitous within calcareous marls (Fig. 5b). These marls/shales are rich in organic carbon (up to 16 wt.% C org ), as evidenced by the dark color in the outcrop ( Fig. 5c and ...
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... tubes are ubiquitous within calcareous marls (Fig. 5b). These marls/shales are rich in organic carbon (up to 16 wt.% C org ), as evidenced by the dark color in the outcrop ( Fig. 5c and ...

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