The mineralization of the structure can be classified as orogenic owing to the finely disseminated nature of the gold, close association with sulfides and deposition within an original bedded organic rich (carbon) sedimentary host (Mikado phyllite).    From Wordnik.com.  [The Earth Times Online Newspaper] Reference

The Alpine orogenic has been quite intense, resulting steep, complex reliefs.    From Wordnik.com.  [South Appenine mixed montane forests] Reference

Despite the orogenic precipitation, the climate of the Tian Shan is strongly continental.    From Wordnik.com.  [Tian Shan montane steppe and meadows] Reference

Of course now that they knew the shield lands were stripped, they'd go right into the nearest orogenic zones.    From Wordnik.com.  [Dinosaur Planet]

The Corsican Mountains belong to the Alpine orogenic system, distinguished by a very complex lithological composition and relief.    From Wordnik.com.  [Corsican montane broadleaf and mixed forests] Reference

Figure 5: After the orogenic stage, weathering and erosion begin removing material from the surface of the newly created mountains.    From Wordnik.com.  [Mountain] Reference

The Cyprus Mountains belong to the Alpine orogenic system, being characterized by a very complex lithological composition and relief.    From Wordnik.com.  [Cyprus Mediterranean forests] Reference

To the north of the pass, the most important orogenic phenomenon occurred at the end of the Pliocene with continuous lifting until the Pleistocene.    From Wordnik.com.  [Eastern Cordillera real montane forests] Reference

In the orogenic stage of mountain building, the accumulated sediments become deformed by compressional forces from the collision of tectonic plates.    From Wordnik.com.  [Mountain] Reference

(You must bear in mind that a weak pull means a correspondingly small density gradient, plus orogenic forces insufficient to raise very tall mountains.).    From Wordnik.com.  [The Rebel Worlds]

Another consequence of the orogenic stage is regional metamorphism and the incursion of magma plumes, plutons, and volcanoes into the growing mountain range.    From Wordnik.com.  [Mountain] Reference

From the geological point of view, the Pindus mountain ranges belong to the Alpine orogenic system, distinguished by a very complex lithological composition.    From Wordnik.com.  [Pindus Mountains mixed forests] Reference

From the geological point of view, the Iberian mountain ranges belong to the Alpine orogenic system, being composed of a very complex lithological composition.    From Wordnik.com.  [Iberian conifer forests] Reference

Intense volcanic and orogenic activity has allowed the formation of many fluvial deposits; the soils in this region are important in their ability to retain water.    From Wordnik.com.  [Trans-Mexican Volcanic Belt pine-oak forests] Reference

This basement was formed during different orogenic phases characterized by large and long-lasting tectonic thermal events that occurred repeatedly during Archean and Proterozoic times.    From Wordnik.com.  [Guyanan savanna] Reference

His principal research focuses on the geodynamics and tectonics of the south Aegean, the exhumation processes of HP rocks, tectonic geomorphology in modern orogenic zones, and basin development.    From Wordnik.com.  [Meet the Team « Interactive Dig Crete – Zominthos Project] Reference

This model suggests that mountain building involves three stages: (1) accumulation of sediments, (2) an orogenic period of rock deformation and crustal uplift, and (3) a period of crustal uplift caused by isostatic rebound and block-faulting.    From Wordnik.com.  [Mountain] Reference

From the geological point of view, the Crete mountain ranges belong to the Alpine orogenic system, characterized by the predominance of Mesozoic and Tertiary sedimentary rocks such as crystalline limestone, marl, sandstone, and conglomerates.    From Wordnik.com.  [Crete Mediterranean forests] Reference

This quaternary plain was formed by the post-orogenic clastic depositing of sediment, derived from adjacent tectonic uplifts deposited in the basin of the lower Magdalena River that formed a platform of peat intercalated with sand and clay beds.    From Wordnik.com.  [Magdalena-Santa Marta mangroves] Reference

The whole sequence of events from the first orogenic movements to the final upheaval in.    From Wordnik.com.  [The Birth-Time of the World and Other Scientific Essays] Reference

If they want to resurrect geosynclinal theory for the formation of orogenic belts - go for it.    From Wordnik.com.  [Clastic Detritus] Reference

Shrinking and splitting of drainage basins in orogenic landscapes from the migration of the main drainage divide.    From Wordnik.com.  [Naturejobs - All Jobs] Reference

These findings support the hypothesis that crustal flow can occur in orogenic belts and contribute to uplift of plateaux.    From Wordnik.com.  [Naturejobs - All Jobs] Reference

It is, in short, indisputable that the orogenic movements which uplift the hills have been at the basis of geological history.    From Wordnik.com.  [The Birth-Time of the World and Other Scientific Essays] Reference

Core logging and gold distribution shows a strong structural control on the high-grade lodes at depth consistent with orogenic gold deposits.    From Wordnik.com. Reference

The orogen experienced crustal thickening and high-temperature decompressional melting, resulting in widespread syn - to late-orogenic granitic intrusions.    From Wordnik.com.  [EurekAlert! - Breaking News] Reference

The orogenic event started before 460 million years ago and lasted until at least 420 million years ago, possibly as a result of far-field plate interactions with Gondwanaland.    From Wordnik.com.  [EurekAlert! - Breaking News] Reference

I propose that this mechanism could clarify the drainage-divide migration and topographic asymmetry found in active orogenic mountain ranges, as seen in the Aconquija Range of Argentina.    From Wordnik.com.  [Naturejobs - All Jobs] Reference

Eocene ------ 6,100 m. and assuming that the orogenic forces began their work in the last quarter of the Eocene period, we have a total of 13,400 m. as some measure of the time which elapsed.    From Wordnik.com.  [The Birth-Time of the World and Other Scientific Essays] Reference

While, according to some of the published sections, the uplifting force would seem to have influenced the final results of the orogenic movements, a discussion of its effects would not be profitable.    From Wordnik.com.  [The Birth-Time of the World and Other Scientific Essays] Reference

Intraplate orogenic belts are the most obvious exception to the plate tectonic paradigm, which assumes that plate interiors are rigid and undeformable, and that orogen-scale deformation occurs exclusively at plate margins.    From Wordnik.com.  [EurekAlert! - Breaking News] Reference

The orogenic structure is complicated.    From Wordnik.com.  [East Siberian taiga] Reference