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BaLLatris [955]
1 year ago
15

0.34 pts when extension and normal faulting result in fault blocks separated by high-angle fault planes near the surface, subsid

ing and rotating relative to one another along a common detachment fault, with sloping or non-horizontal strata, these structures are group of answer choices tilted fault blocks horsts and grabens transform blocks reverse faults fold and thrust belts
Geography
1 answer:
ioda1 year ago
8 0

Tilted Fault Blocks also called as Rotational block faulting are the structures that are formed. They are formed in extensional tectonic events where the brittle crust fractures due to extension creating detachment faults and crusts gets tilted.

As tectonic plates separate during extensional tectonic events, tilted block faulting, also known as rotational block faulting, is a mechanism of structural evolution. Detachment faults are produced when extensional pressures are applied to the upper lithospheric crust. These typical faults manifest on a regional scale, with the ductile bottom crust ascending and the higher crust fracturing into tilted fault blocks. As a result, ductile deformed deeper crust is lifted, cooled, and exhumed. The substantial group of slanted blocks and related crust may make up a substantial portion of metamorphic core complexes, which are present in both continental and oceanic crust.

Learn more about Tilted Fault Blocks here:

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What about the united states’ geography would influence their foreign policy until this time?
Sunny_sXe [5.5K]

The united states’ geography would influence their foreign policy until this time

<h3>What is foreign policy?</h3>
  • Geography has been more of an ally than an enemy since the beginning of the nation. An island cannot control an entire continent, as the British discovered.
  • America was undoubtedly exposed in those foreign policy. With their imperial aspirations, the French and Spanish posed a threat to North America.
  • The British also weren't willing to give up easy; in 1812, the king's troops invaded and set fire to areas of Washington, and they did so again during the American Civil War.
  • Nevertheless, for the majority of its history, the United States had a foreign policy unmatched by other nations.

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7 0
2 years ago
Why is it so difficult for<br> scientists to determine how the Jalisco block is<br> moving
NeX [460]

Answer:

Extensional faulting observed in southwestern Mexico has been related to the incipient rifting of the Jalisco block from the Mexican mainland since the Pliocene. On the basis of new structural and geophysical data, we propose that (1) the continental boundaries of the Jalisco block are ancient structures reactivated since the Pliocene at a low (<1 mm/yr) rate of deformation, and (2) Pliocene-Quaternary extensional faulting at the edges of Jalisco block is a basement-controlled intraplate deformation related to plate boundary forces rather than to active continental rifting. The Jalisco block boundaries first developed in response to the uplift of the Puerto Vallarta batholith in pre-Neogene time and underwent a complex contractile deformation before the Pliocene. During Pliocene-Quaternary times north-northeast extension reactivated the northern boundary, forming the Tepic-Zacoalco rift, whereas east-southeast extension formed the northern Colima rift. South of the Colima volcano, active extension is found only west of the so-called southern Colima rift and partly reactivates old northeast-trending basement faults. The parallelism between the subducted Rivera-Cocos plate boundary zone and the eastern neotectonic boundary of the Jalisco block supports eastsoutheastward motion of the southern Mexican blocks induced by the differential motion and oblique subduction of the Cocos and Rivera plates. On the other hand, we envisage Pliocene-Quaternary extension along the northern boundary as an upper-plate response to the low convergence rate and the steep subduction angle of the Rivera plate.

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algol [13]

Answer:

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