In the example
of orogeny, things which are probably well known to specialists in Chinese orogony, but not to experts in orogony in general, let alone all geologists are referenced.
The anomalous magnetic signal is consistent with an older tectonic event — the
Alleghanian orogeny that formed the Alleghany - Appalachian Mountains when the supercontinent of Pangea was assembled.
The result of this collision was what is known as the
Variscan orogeny, the raising of a mountain range along the North - South axis, which left the rocks with a secondary magnetic signal, adapted to the new magnetic field of the Earth.
«When we dated the ruby deposits, we noticed that they were directly related to the continental collision and to the
Himalayan orogeny [mountain building],» says Giuliani.
These fractures lie along the structural axes of the island itself, forming themselves from the
Alpine orogeny during the Tertiary Period due to the movements of the African plate.
A period of mountain - building was also underway (the so - called
Taconic orogeny) increasing the amount of rock weathering taking place and subsequently lowering CO2 levels even further.
Also, it shows graphically the distribution of earthquakes by their magnitude and frequency that are caused by movement in
the orogeny — a belt of the earth's crust involved in the formation of mountains.
He points out that this magnetic signal can be associated with large - scale processes of mountain formation, and how these ranges can be curved until they create structures known as oroclines: «With a rock sample, we can analyse a process that has occurred on the tectonic plate level; and, specifically, offers new data that allows us to discover how
this orogeny or large Variscan range and its curvature occurred.
Also, it shows graphically the distribution of earthquakes by their magnitude and frequency that are caused by movement in
the orogeny - a belt of the earth's crust involved in the formation of mountains.
Even such recently developed theories as plate tectonics are not referenced in papers discussing issues centrally related to it (eg,
orogeny).