Synsedimentary ash rains and paleoenvironmental conditions during the deposition of the Chachil Formation (Pliensbachian) at its type locality, Neuquén Basin, Argentina
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文摘

Sedimentological analyses validate Chachil Fm instead of Chachil Limestones.

Deposition occurred in a shallow mixed volcaniclastic-carbonate platform.

The carbonate platform sedimentation was affected by ash fall supply.

Primary pyroclastic and resedimented tuffolitic facies were recognized.

Zircon U-Pb ages reveal a Pliensbachian tephra input affecting the platform.

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