scispace - formally typeset
Search or ask a question

How fast can metamorphic rocks be exhumed? 


Best insight from top research papers

Metamorphic rocks can be exhumed at rates comparable to plate tectonic speeds. The exhumation rates of ultrahigh-pressure rocks in the Neoproterozoic and modern collisional orogens have been found to be fast, with average vertical exhumation rates of 0.9 ± 0.3 cm/yr . Exhumation of high-pressure metamorphic rocks can occur with typical plate velocities of cm/year, driven by forced flow in a subduction channel . The exhumation rates of the deepest subducted Alpine rocks have been estimated to be 3.4 cm/yr and 1.6 cm/yr, indicating fast exhumation at plate tectonic speeds . The metamorphic evolution of ultrahigh-pressure garnet peridotite from Alpe Arami suggests extremely fast exhumation rates of c. 15 mm yr−1 or more . Exhumation of amphibole-eclogite facies rocks in the California Coast Ranges occurred as a single episode with fast and uniform exhumation rates up to ~140°C/Ma .

Answers from top 5 papers

More filters
Papers (5)Insight
The paper provides evidence that metamorphic rocks can be exhumed at extremely fast rates of approximately 15 mm/yr or more.
The paper provides evidence that metamorphic rocks in the California Coast Ranges were exhumed at fast rates of up to ~140°C/Ma during a one-time event.
Journal ArticleDOI
Daniela Rubatto, Joerg Hermann 
01 Jan 2001-Geology
485 Citations
The paper provides evidence that the exhumation of deeply buried metamorphic rocks can occur at rates of 3.4 cm/yr and 1.6 cm/yr, which is similar to the speed of subduction.
The paper states that the maximum exhumation rate for metamorphic rocks in subduction channels is approximately 1/3 of the subduction burial rate.
The paper provides evidence that the exhumation rate of ultrahigh-pressure rocks in the West Gondwana orogen was approximately 0.9 ± 0.3 cm/yr, which is considered fast.

Related Questions

Did the maya perform exhumation in jaina island?4 answersThe Maya did perform exhumation in Jaina Island. The site of Jaina Island is unique due to its specially developed burial culture involving ceramic figurines. These figurines are found in graves, unlike other Maya sites where they are mostly found in domestic contexts. The exhumation process in Jaina Island is believed to have been performed by the formation of a D2 extrusion wedge made up of metamorphic rocks. This wedge had a subduction thrust as its base and a detachment fault as its roof. The exhumation was related to the Eocene ridge subduction, which caused a high thermal gradient during ridge subduction and resulted in the exhumation of the metamorphic rocks.
Where do people exhume the bones of their ancesters?5 answersPeople exhume the bones of their ancestors in various locations such as burial grounds, home courtyards, open land, ditches, rubbish dumps, and even during excavations for new constructions.
Where in the americas people exhume the bones of their ancesters?4 answersExhumation of ancestral bones is practiced in several countries in the Americas. In Latin America, exhumation processes have been carried out in Guatemala, El Salvador, Colombia, Peru, Chile, Argentina, Uruguay, Brazil, Paraguay, Venezuela, Mexico, Panama, Ecuador, and Honduras. These exhumations are a result of various events such as collective massacres, state policies leading to disappearances, collective violence, and selective deaths under democratic regimes. The exhumation process in Latin America is seen as a part of transitional justice and has implications for the social and political life of these exhumed corpses in post-conflict societies. In North America, repatriation of American Indian bones from museums, universities, and historical societies is a major concern for tribal groups. The repatriation issue arises due to differing cultural concepts of the body and has gained prominence recently.
How can we automate the discovery of metamorphic relations?5 answersAutomating the discovery of metamorphic relations can be achieved by extracting and generalizing encoded metamorphic relations from existing test cases in open-source software projects. This approach has been proposed in papers by Xu et al.and Müller et al.. The proposed method, called MR-Extractor, identifies test cases that encode metamorphic relations in open-source software and then generalizes these relations into parameterized methods for metamorphic testing. The reusability of these codified metamorphic relations for new test generation is validated. Experimental results show that MR-Extractor can identify a significant number of metamorphic relation-encoded test cases and that test cases constructed from these relations can effectively improve test coverage. The approach has been evaluated in various domains, including computational material scienceand query-based systems.
How fast can we search ?5 answersThe speed at which we can search depends on various factors such as the efficiency of the search algorithm, the size of the dataset, and the computational resources available. Efficient search algorithms, such as binary search or hash-based search, can significantly reduce the search time by quickly narrowing down the search space. Additionally, parallel processing techniques can be employed to distribute the search workload across multiple processors or machines, further improving search speed. The size of the dataset also plays a crucial role, as larger datasets require more time to search through. Finally, the computational resources available, such as processing power and memory, can impact search speed. With more powerful hardware, searches can be performed faster. Overall, the speed of searching is a complex interplay between algorithm efficiency, dataset size, and available computational resources.
What is the rate of plate tectonics movement?4 answersThe rate of plate tectonics movement is steady and can be measured over several years or several million years. Recent studies of the motion of the Pacific and North American plates suggest that plate tectonic motion averaged over these time scales is consistent. The speed of plate movement can be deduced through analysis of magnetic anomalies above mid-ocean ridges, where the direction of the geomagnetic field is frozen into the crust formed by cooling magma. Rates of motion are determined by the spacing between dated magnetic highs and lows. Additionally, plate tectonic reconstruction approaches can extract time-dependent plate velocities and geometries, providing a median root mean square (RMS) plate speed of approximately 4 cm/yr over 200 million years. The motion of oceanic plates tends to be 2-3 times faster than continental plates, and plates with large continental fractions have slower RMS velocities.

See what other people are reading

Examples of metamorphic reactions?
5 answers
WHERE does Rock fall happend in Limpopo?
5 answers
Examples of metamorphic reactions?
5 answers
WHERE does Rock fall happend in Limpopo?
5 answers
How does Nd/Sm radiometric dating in pegmatites?
4 answers
Nd/Sm radiometric dating in pegmatites involves analyzing the Sm-Nd isotope systematics of minerals like garnet, monazite, and apatite to determine the age of formation. Pegmatites from different regions exhibit varying Nd isotopic compositions, indicating diverse sources. For instance, pegmatites in Maine show distinct Nd isotopic characteristics between different series. In the Eastern Alps, garnet Sm-Nd data from various rock types reveal challenges like high-LREE inclusions and isotopic disequilibrium, emphasizing the need for careful evaluation. Additionally, pegmatites in Antarctica provide insights into the cooling history of rocks based on Sm-Nd and Rb-Sr ages. Overall, Nd/Sm radiometric dating in pegmatites helps unravel the geological history, source characteristics, and metamorphic events associated with these unique rock formations.
What is the Madukkarai Wall?
4 answers
The Madukkarai Wall refers to a significant geological feature in the Madurai Block of the Southern Granulite Terrane in Peninsular India. This region comprises three sub-blocks: the Neoarchean Northern Madurai block, Paleoproterozoic Central Madurai block, and the Neoproterozoic Southern Madurai Block. The Madurai Block hosts ultrahigh-temperature (UHT) granulite facies rocks, including a layered mafic-ultramafic intrusion found in association with Mg-Al granulites at Ganguvarpatti in the Central Madurai Block. The area is also characterized by the Suruli shear zone, a ductile shear zone extending over 150 km from Kadaiyanallur to Ganguvarpatti, showcasing transposed foliation and mylonite foliation. This geological setting is crucial for understanding the tectonic evolution and magmatic history of the region within the broader context of the Gondwana supercontinent.
What is monazite?
5 answers
Monazite is a significant accessory mineral used in dating geological processes due to its internal structure, which can be observed through cathodoluminescence (CL) techniques. It contains thorium (Th), uranium (U), and rare earth elements (REEs) and is challenging to study using isotope research methods. Monazite's chemical dating reveals ages, such as a Triassic age for monazite from lithium-bearing granitic pegmatites. Monazite in pelitic granulites records Paleoproterozoic metamorphism and Triassic fluid modification, indicating complex geological histories. Monazite is also considered for nuclear power generation due to its Th and U content, with ongoing research focusing on high-temperature cracking processes for efficient cation liberation.
What is the population to a place called Eastern kaapval craton?
5 answers
The Eastern Kaapvaal Craton is characterized by a complex geological history, with significant crustal evolution spanning from 3.66 to 2.67 billion years ago. The region exhibits a variety of rock formations, including tonalite–trondhjemite–granodiorite (TTG) association and greenstone belts, with extensive tectono-magmato-metamorphic events shaping its geological features. Mesoarchean magmatism in the area is linked to volcanic sequences like the Usushwana Igneous Complex and the Hlagothi Complex, providing insights into the mantle sources and genetic relations of these rocks. The construction and stabilization of the Eastern Kaapvaal Craton involved terrane assembly, subduction, and granitic intrusions around 3.3–3.1 billion years ago, followed by tectonic movements and erosion processes until approximately 2.9 billion years ago. Geochronological data from the region helps in understanding the development and evolution of the Kaapvaal Craton over time.
Whole rock analysis for geochemistry of adakites methodology
5 answers
Whole rock analysis for the geochemistry of adakites involves examining various geochemical characteristics. Adakites typically exhibit low MgO and Mg# values, high Sr/Y and La/Yb ratios, high Zr/Sm ratios, high Na2O contents, and specific 87Sr/86Sr ratios, indicating their adakitic affinity. Discriminant analysis can help classify adakites based on their chemical composition, distinguishing between different geodynamic settings. Studies have shown that adakitic melts are rare compared to adakitic rocks, with only a small percentage identified in large databases, suggesting a complex relationship between adakitic rocks, adakitic melts, and plate melting processes. Additionally, the formation of high-Mg# adakitic rocks may involve garnet fractionation in mantle-derived magmas, with specific mineralogical evidence supporting this process.
Albite, clinochlore, quartz, and anorthite, what stone form?
5 answers
Albite, clinochlore, quartz, and anorthite collectively form a variety of mineral assemblages under different geological conditions. Albite can break down to jadeite and quartz at high pressure, while anorthite can undergo incongruent melting to corundum and liquid at specific pressures. Additionally, albite can be part of alteration processes, transitioning to albitite with increasing intensity of albitic alteration. In metamorphic settings, albite can coexist with anorthite in amphibole schists, indicating stability at low metamorphic grades. Furthermore, albite can be found in aluminosilicate glasses synthesized through hydrothermal methods, where the addition of water induces structural changes by breaking down the linkage of tetrahedra to form clusters. Therefore, these minerals collectively contribute to diverse mineralogical compositions in various geological settings.
What are the chemical reactions involved in the chloritization of biotite?
4 answers
The chloritization of biotite involves several key chemical reactions. Biotite chloritization reactions include the inflow of Al3+, Fe2+, Mn2+, and Mg2+ ions, and the outflow of H4SiO4, Ca2+, K+, and F– ions. The process leads to a gradual decrease in aluminum, iron, manganese, and magnesium ions in the hydrothermal fluid, while calcium, hydrogen, and fluorine ions increase gradually as chloritization progresses. Additionally, the formation of chlorite from biotite involves two essential mechanisms: one with a small volume decrease and significant inflow of metallic ions, and the other with a large volume decrease and outflow of metallic ions into the hydrothermal fluid. These reactions not only drive the chloritization process but also influence the physicochemical parameters of the hydrothermal fluid, such as pH and redox potential, as chloritization advances.