In geology, terrane is a shortened term for tectonostratigraphic terrane. Examples of a terrane would be Lhasa Terrane in Tibet and Pearya Terrane in the United States.
The Franciscan terrane in California is an example of a terrane. It is a complex geologic region characterized by a diverse assemblage of rocks that were accreted to the North American continent during the Mesozoic era.
"Terrain" refers to a topographic or geographic landscape configuration--for example, a "hilly terrain," or a "wooded terrain." "Terrane" refers to a lighologic or geologic areal expanse--for example, a "metamorphic terrane," or a "basaltic terrane."
Terrane
At the boundaries of a terrane, you can find faults, shear zones, and deformation zones where the terrane has been accreted or sutured onto adjacent tectonic plates. These boundaries may exhibit complex structures due to the collision and deformation processes that have occurred as the terrane was incorporated into the larger tectonic framework.
A terrane is a fragment of crust that has a geologic history different from that of the surrounding crust, often resulting from tectonic movements.
The Franciscan terrane in California is an example of a terrane. It is a complex geologic region characterized by a diverse assemblage of rocks that were accreted to the North American continent during the Mesozoic era.
"Terrain" refers to a topographic or geographic landscape configuration--for example, a "hilly terrain," or a "wooded terrain." "Terrane" refers to a lighologic or geologic areal expanse--for example, a "metamorphic terrane," or a "basaltic terrane."
Jacques Terrane's birth name is Jacques Tartire.
It is called a terrane (more specifically, a tectonostratigraphic terrane). An example of these sutured chunks of oceanic plate is found in south central South Carolina.
Terrane
Jacques Terrane was born on August 23, 1915, in Paris, France.
Alain Terrane was born on July 17, 1923, in Bandol, Var, France.
Alain Terrane died on February 28, 2000, in Mougins, Alpes-Maritimes, France.
At the boundaries of a terrane, you can find faults, shear zones, and deformation zones where the terrane has been accreted or sutured onto adjacent tectonic plates. These boundaries may exhibit complex structures due to the collision and deformation processes that have occurred as the terrane was incorporated into the larger tectonic framework.
The lithology, age, fossils, and paleomagnetic orientation of a suspect terrane may differ from its host continent.
A terrane is a fragment of crust that has a geologic history different from that of the surrounding crust, often resulting from tectonic movements.
A terrane is a distinct crustal block that has a geologic history separate from the surrounding area, often brought in from elsewhere by plate tectonics. This means that the rocks, structures, and geologic history of a terrane can differ significantly from the surrounding area.