Prediction of ultrathin lacustrine sandstones by joint investigation of tectonic geomorphology and sedimentary geomorphology using seismic data
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文摘

Paleogeomorphologic elements on Cretaceous unconformity were reconstructed.

Seismic lithology of 1–7 m thick sandstones was realized using 90° seismic traces.

Amplitude stratal slices illustrate lobate sedimentary geomorphologic patterns and sandstone thickness trends.

The agreement between above elements reduces uncertainties of mapping ultrathin sandstone reservoirs.

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