Examples of interbedded

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There are black mudstones interbedded with the siltstones.
The channelized sandstones are overlain by medium to thick sandstone beds and thin interbedded mudstones.
Interbedded thin fine-grained sandstone and siltstone layers are laminated and wavy in nature.
Upwardthinning and -fining cycles were recognized, but the interbedded marine strata were not.
The lower member (max. c. 600 m) is composed mainly of thick clay shales interbedded with thin sandy limestone beds (packstones and wackestones).
Occasionally 1-1.5 m thick, rippled fine-grained sandy units are seen overlying this interbedded assemblage with a sharp contact.
Tuffs interbedded within interfluvially driven sediments, often cross-laminated fine- to medium-grained sandstones, display both current- and tool-marks.
These sediments are locally interbedded with siliceous limestone and rare thin-bedded sandstones.
The latter was described as "massive sandstones and conglomerates with interbedded sandy shales which are of continental origin".
Depleted olivine basalts are associated with radiolarian cherts while most pelagic limestones and cherts are found interbedded with alkali basalts.
Individual radiolarian chert beds range in thickness from 3-4 cm thick and are interbedded with shale or mudstone.
Bioturbation is common, but occurs almost exclusively in the interbedded mudstones: 23 % of mudstone beds contain bioturbation, compared with 1.6 % of the sandstones.
Simultaneous eruption of ash-flow tuffs resulted in a sequence of interbedded tuffs, sedimentary breccias and andesitic lavas.
Interbedded shale and coal facies contain occasional desiccation cracks and locally gypsum crystals.
The ore and interbedded sediments contain filamentous microfossils up to 60 mm wide, and spheroidal microfossils 7-14 mm wide with a single aperture.

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