anticlinal

Oil has pooled at the top of the anticlinal fold for each unit.

In this second anticlinal ridge, the sediments already show a thickness of 1000 m.

The center of the Negev is dominated by northeast-southwest anticlinal ridges.

The system of anticlinal ridges affecting the sedimentary cover is also arranged in this direction.

Hanging Rocks consists of anticlinal stratified sandstone and limestone layers.

The mountain has an anticlinal shape and is almost completely composed of mesozoic limestone formations.

Anticlinal structures formed by inversion provide traps in many of the world's hydrocarbon provinces.

The mountain is anticlinal in structure.

Overall the field is an anticlinal structure somewhat akin to a dome, with its axis running northwest to southeast.

It is an anticlinal structure, with oil trapped stratigraphically by the anticline.

It is in an anticlinal dome.

This is an anticlinal range within the body of the mountain system with flanking strata rising well on the slopes.

The Southern Range forms the third anticlinal uplift.

The field is a faulted anticlinal structure with oil trapped by a combination of structural and stratigraphic mechanisms.

An anticlinorium is a series of anticlinal folds on a regional-scale anticline.

The observed anticlinal "skewed" shape is a compromise between two conformers, called syn and anti.

Particularly noticeable are the numerous plunging anticlinal noses at the northeastern end of the Smoke Holes.

The occupancy of this area causes displacement above the detachment in the form of material migration to the anticlinal core.

Secondly, it has been suggested a fault may propagate into the anticlinal core if material flow and accommodation space are not at equilibrium.

Other fungi tend to form appressoria over anticlinal cell walls and some form them at any location.

Valleys may be synclinal valleys or anticlinal valleys.

Anticlinal divisions are likely while periclinal and oblique divisions are definitive.

Whilst the regional dip of the rock beds is to the south, locally they vary and a broad anticlinal structure coincides with the hill.

In the North Belridge Field, most oil is trapped in anticlinal formations.

The sediments are affected by a series of large, mainly anticlinal folds that show a variety of trends in the central part of the island.