Relevant bibliographies by topics / Plate tectonics – Himalaya Mountains

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Plate tectonics – Himalaya Mountains'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 January 2023

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Journal articles on the topic "Plate tectonics – Himalaya Mountains"

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Morley, Robert J. "Assembly and division of the South and South-East Asian flora in relation to tectonics and climate change." Journal of Tropical Ecology 34, no. 4 (2018): 209–34. http://dx.doi.org/10.1017/s0266467418000202.

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Abstract:The main phases of plant dispersal into, and out of the South-East Asian region are discussed in relation to plate tectonics and changing climates. The South-East Asian area was a backwater of angiosperm evolution until the collision of the Indian Plate with Asia during the early Cenozoic. The Late Cretaceous remains poorly understood, but the Paleocene topography was mountainous, and the climate was probably seasonally dry, with the result that frost-tolerant conifers were common in upland areas and a low-diversity East Asian aspect flora occurred at low altitudes. India's drift into
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Feng, Han, Huayu Lu, Barbara Carrapa, et al. "Erosion of the Himalaya-Karakoram recorded by Indus Fan deposits since the Oligocene." Geology 49, no. 9 (2021): 1126–31. http://dx.doi.org/10.1130/g48445.1.

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Abstract The Cenozoic erosion history of the Himalaya-Karakoram, which is a function of tectonically driven uplift and monsoon climatic evolution in South Asia, remains elusive, especially prior to the Miocene. Here, we present a multiproxy geochemical and thermochronological analysis of the oldest samples available from the Arabian Sea, which we used to investigate the erosion history of the Himalayan and Karakoram orogenic system. The Indus Fan records rapid and sustained erosion of the Himalayan-Karakoram mountains from before 24 Ma (ca. 30) to ca. 16 Ma concurrent with changing provenance
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Manish, Kumar, and Maharaj K. Pandit. "Geophysical upheavals and evolutionary diversification of plant species in the Himalaya." PeerJ 6 (November 7, 2018): e5919. http://dx.doi.org/10.7717/peerj.5919.

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The Himalaya is one of the youngest and the loftiest mountain chains of the world; it is also referred to as the water tower of Asia. The Himalayan region harbors nearly 10,000 plant species constituting approximately 2.5% of the global angiosperm diversity of which over 4,000 are endemics. The present-day Himalayan flora consists of an admixture of immigrant taxa and diversified species over the last 40 million years. The interesting questions about the Himalayan flora discussed here are: how did the Himalaya achieve high endemic plant diversity starting with immigrant taxa and what were the
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Yangshen, Shi, Jia Chengzhao, Jia Dong, and Guo Lingzhi. "Plate tectonics of East Qinling Mountains, China." Tectonophysics 181, no. 1-4 (1990): 25–30. http://dx.doi.org/10.1016/0040-1951(90)90006-t.

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SHAH, Afroz Ahmad, and Nurhafizah MANAN. "Gravitational Tectonics versus Plate Tectonics in the Himalayan Intermontane Basins: NW Himalaya." Acta Geologica Sinica - English Edition 95, S1 (2021): 3–6. http://dx.doi.org/10.1111/1755-6724.14813.

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Şahin, Şakir, and Jülide Parlak. "The Determination of Subduction Geometry under the Aegean-Anatolian Plate along Aegean and Cyprean Arcs in the Eastern Mediterranean." International Journal of Advanced Engineering and Management Research 07, no. 04 (2022): 80–104. http://dx.doi.org/10.51505/ijaemr.2022.7407.

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The southwestern Anatolia is part of the Aegean extensional province, located in a seismically active convergent zone between the African and Eurasian Plates in the Eastern Mediterranean. This region is one of the most active and swiftly deforming domains of the Alpine–Himalayan mountain belt in Turkey. The plate boundary is shaped by the subduction of the African Plate under the Aegean-Anatolian plate consists of the Aegean and Cyprean arcs. The two separate slabs occurred along the plate border related to these arcs. These subducted slabs are separated by a gap beneath Western Anatolia. Thes
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Thakur, V. C., R. Jayangondaperumal, and V. Joevivek. "Seismotectonics of central and NW Himalaya: plate boundary–wedge thrust earthquakes in thin- and thick-skinned tectonic framework." Geological Society, London, Special Publications 481, no. 1 (2018): 41–63. http://dx.doi.org/10.1144/sp481.8.

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AbstractThe tectonic framework of NW Himalaya is different from that of the central Himalaya with respect to the position of the Main Central Thrust and Higher Himalayan Crystalline and the Lesser and Sub Himalayan structures. The former is characterized by thick-skinned tectonics, whereas the thin-skinned model explains the tectonic evolution of the central Himalaya. The boundary between the two segments of Himalaya is recognized along the Ropar–Manali lineament fault zone. The normal convergence rate within the Himalaya decreases from c. 18 mm a−1 in the central to c. 15 mm a−1 in the NW seg
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Khan, Zahid Ali, Ram Chandra Tewari, and Rabindra Nath Hota. "Problems in Accepting Plate Tectonics and Subduction as a Mechanism of Himalaya Evolution." IOSR Journal of Applied Geology and Geophysics 05, no. 03 (2017): 81–100. http://dx.doi.org/10.9790/0990-05030181100.

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Hughes, Nigel C., and Peter A. Jell. "Cambrian trilobite faunas from India: a multivariate and computer-graphic reappraisal and its paleogeographic implications." Paleontological Society Special Publications 6 (1992): 141. http://dx.doi.org/10.1017/s2475262200007012.

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Cambrian trilobite faunas from northern India provide data critical for assessing earliest Phanerozoic paleogeography and for constraining tectonic models of Himalayan evolution. Previous investigations suggest that Indian Middle Cambrian trilobite faunas, collected from basins 500 km apart, are strikingly different. The Kashmir fauna, in the west, shows supposed faunal affinities with northern China, while the Spiti fauna, in the east, was considered of European affinity. This counterintuitive faunal distribution in adjacent basins might suggest that the area was made up of several micro-cont
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Wan, Bo, Xusong Yang, Xiaobo Tian, Huaiyu Yuan, Uwe Kirscher, and Ross N. Mitchell. "Seismological evidence for the earliest global subduction network at 2 Ga ago." Science Advances 6, no. 32 (2020): eabc5491. http://dx.doi.org/10.1126/sciadv.abc5491.

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The earliest evidence for subduction, which could have been localized, does not signify when plate tectonics became a global phenomenon. To test the antiquity of global subduction, we investigated Paleoproterozoic time, for which seismic evidence is available from multiple continents. We used a new high-density seismic array in North China to image the crustal structure that exhibits a dipping Moho bearing close resemblance to that of the modern Himalaya. The relict collisional zone is Paleoproterozoic in age and implies subduction operating at least as early as ~2 billion years (Ga) ago. Seis
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Dissertations / Theses on the topic "Plate tectonics – Himalaya Mountains"

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Holt, William Everett. "The active tectonics and structure of the Eastern Himalayan Syntaxis and surrounding regions." Diss., The University of Arizona, 1989. http://hdl.handle.net/10150/184802.

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I determined the source parameters of 53 moderate-sized earthquakes in the region of the Eastern Himalayan Syntaxis through the joint inversion of regional and teleseismic distance long-period body waves. The average rates of deformation are determined by summing the moment tensors from both recent and historic earthquakes. Strike-slip movement on the Sagaing fault terminates in the north (just south of the syntaxis), where thrusting (northeast convergence) and crustal thickening are predominant. Slip vectors for thrust mechanisms in the Eastern Himalaya in general are not orthogonal to the Hi
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Chan, Yau-cheong Ian, and 陳有昌. "Characterizing crustal melt episodes in the Himalayan orogen." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/206505.

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Extensive studies have been undertaking in exploring the tectonic evolution of the Himalayan Orogen. Various tectonic models were developed to explain and constraint spatially and temporally critical events including the collision of Indian Plate with the Eurasia Plate, crustal thickening in association with the indentation, crustal spreading of the Tibetan Plateau. Recent study by King et al., 2011 identified two distinct leucogranite suites which were formed by contrasting tectonic actions at Sakya. They are Equigranular Anastomosing Leucogranite (AEG) formed under prograde fluidpresent cond
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Sattarzadeh-Gadim, Yosef. "Active tectonics in the Zagros Mountains, Iran." Thesis, Imperial College London, 1997. http://hdl.handle.net/10044/1/7922.

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Rigby, Michael Gomez Francisco Gustavo. "Recent faulting and active shortening of the Middle Atlas Mountains, Morocco, within the diffuse African-Eurasian plate boundary." Diss., Columbia, Mo. : University of Missouri-Columbia, 2008. http://hdl.handle.net/10355/5796.

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Thesis (M.S.)--University of Missouri-Columbia, 2008.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed on July 8, 2009) Includes bibliographical references.
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Williams, Helen Myfanwy. "Magmatic and tectonic evolution of Southern Tibet and the Himalaya." Thesis, [n.p.], 2000. http://library7.open.ac.uk/abstracts/page.php?thesisid=58.

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Cai, Keda, and 蔡克大. "Magmatism and tectonic evolution of the Chinese Altai, NW China: insights from the paleozoic mafic andfelsic intrusions." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B47147192.

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WUST, STEPHEN LOUIS. "TECTONIC DEVELOPMENT OF THE PIONEER STRUCTURAL COMPLEX, PIONEER MOUNTAINS, CENTRAL IDAHO (CORE, DETACHMENT, EXTENSION)." Diss., The University of Arizona, 1986. http://hdl.handle.net/10150/183813.

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The Pioneer Mountains of Idaho expose a lower plate core of Precambrian and Ordovician metasedimentary rocks, which are intruded by Cretaceous and Eocene plutonic bodies. The core is separated by a detachment fault from a surrounding upper plate of Paleozoic and Tertiary sedimentary and volcanic units. The detachment system developed during a Tertiary extensional event which overprinted Paleozoic and Mesozoic east-directed compressional features, and exhibits both brittle and ductile (mylonitic) deformation. Stretching lineations in the mylonite and striations along the detachment surface both
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Bemis, Sean Patrick 1979. "Moletrack scarps to mountains: Quaternary tectonics of the central Alaska Range." Thesis, University of Oregon, 2010. http://hdl.handle.net/1794/10563.

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xvi, 121 p. : ill. (some col.), maps (some col.) Also includes two large-scale maps in two separate pdf files. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number.<br>Deformation across plate boundaries often occurs over broad zones with relative motions between plates typically accommodated by faults of different styles acting together in a complex system. Collision of the Yakutat microplate within the Alaskan portion of the Pacific-North America plate boundary drives deformation over 600 km away where the Denali fau
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Cunningham, William Dickson 1960. "Superposed thrusting in the northern Granite Wash Mountains, La Paz County, Arizona." Thesis, The University of Arizona, 1986. http://hdl.handle.net/10150/558059.

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Janecke, Susanne Ursula 1959. "Structural geology and tectonic history of the Geesaman Wash area, Santa Catalina Mountains, Arizona." Thesis, The University of Arizona, 1986. http://hdl.handle.net/10150/558061.

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Books on the topic "Plate tectonics – Himalaya Mountains"

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Geology and tectonics of the Karakoram Mountains. Wiley, 1991.

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Colliding continents: A geological exploration of the Himalaya, Karakoram, & Tibet. Oxford University Press, 2013.

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3

Asif, Khan M., and Geological Society of London, eds. Tectonics of the Nanga Parbat syntaxis and the Western Himalaya. Geological Society, 2000.

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4

Group, Meeting on "Seismotectonics and Geodynamics of the Himalaya" (1995 Dept of Earth Sciences University of Roorkee). Geodynamics of the NW Himalaya. Field Science Publishers, 1999.

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Mascle, Georges H. Himalaya-Tibet: La collision continentale Inde-Eurasie. Vuibert, 2010.

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Malkin, Carolyn Arden. Mountains and valleys. Chelsea House, 2009.

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Arden, Carolyn. Mountains and valleys. Chelsea House, 2009.

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Gravity field, seismicity, and tectonics of the Indian peninsula and the Himalayas. D. Reidel Pub. Co., 1985.

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ill, Schindler S. D., ed. As old as the hills. F. Watts, 1989.

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10

Girard, Matthieu. Metamorphism and tectonics of the transition between non metamorphic Tethayan Himalaya sediments and the North Himalayan Crystalline Zone (Rupshu area, Ladakh, NW India). Section des sciences de la terre, Institut de géologie et paléontologie, Université de Lausanne, 2001.

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Book chapters on the topic "Plate tectonics – Himalaya Mountains"

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Thakur, V. C., M. Joshi, and R. Jayangondaperumal. "Active Tectonics of Himalayan Frontal Fault Zone in the Sub-Himalaya." In Geodynamics of the Indian Plate. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-15989-4_12.

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Jiracek, George R., Victor M. Gonzalez, T. Grant Caldwell, Philip E. Wannamaker, and Debi Kilb. "Seismogenic, electrically conductive, and fluid zones at continental plate boundaries in New Zealand, Himalaya, and California." In A Continental Plate Boundary: Tectonics at South Island, New Zealand. American Geophysical Union, 2007. http://dx.doi.org/10.1029/175gm18.

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Molnar, Peter. "6. Tectonics of continents." In Plate Tectonics: A Very Short Introduction. Oxford University Press, 2015. http://dx.doi.org/10.1093/actrade/9780198728269.003.0006.

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‘Tectonics of continents’ shows that the much greater thickness of continental than oceanic crust makes continental and oceanic lithosphere behave differently. First, because crust is less dense and therefore buoyant, compared with the mantle, thick continental crust resists subduction into the asthenosphere. Slices of the upper part of the crust detach from underlying parts and become stacked atop one another to form a mountain range, like the Alps or Himalaya. Second, continental lithosphere is weaker than oceanic lithosphere and when put under stress it deforms. When the horizontal dimension of a region of continental crust is shortened, the crust thickens. Because of isostasy, thick buoyant crust stands higher than thin crust, creating mountain ranges. Various mountain ranges around the world are used to illustrate these principles.
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Adlakha, Vikas, and Kalachand Sain. "Crustal Evolution of the Himalaya since Paleoproterozoic." In Earth’s Crust and Its Evolution - From Pangea to the Present Continents [Working Title]. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.104259.

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Understanding the crustal evolution of any orogen is essential in delineating the nomenclature of litho units, stratigraphic growth, tectonic evolution, and, most importantly, deciphering the paleogeography of the Earth. In this context, the Himalayas, one of the youngest continent-continent collisional orogen on the Earth, has played a key role in understanding the past supercontinent cycles, mountain building activities, and tectonic-climate interactions. This chapter presents the journey of Himalayan rocks through Columbian, Rodinia, and Gondwana supercontinent cycles to the present, as its litho units consist of the record of magmatism and sedimentation since ~2.0 Ga. The making of the Himalayan orogen started with the rifting of India from the Gondwanaland and its subsequent movement toward the Eurasian Plate, which led to the closure of the Neo-Tethyan ocean in the Late-Cretaceous. India collided with Eurasia between ∼59 Ma and ∼40 Ma. Later, the crustal thickening and shortening led to the metamorphism of the Himalayan crust and the development of the north-dipping south verging fold-and-thrust belt. The main phase of Himalayan uplift took place during the Late-Oligocene-Miocene. This chapter also provides insights into the prevailing kinematic models that govern the deep-seated exhumation of Himalayan rocks to the surface through the interplay of tectonics and climate.
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Gupta, Avijit. "Landforms of Southeast Asia." In The Physical Geography of Southeast Asia. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199248025.003.0013.

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Southeast Asia is a corner of the continent of Asia which ends in an assemblage of peninsulas, archipelagos, and partially enclosed seas. Towards the northwest, the physical contact of this region with the rest of Asia is via a mountainous region that includes the eastern Tibetan Plateau, the eastern Himalaya Mountains, the hills and plateaux of Assam (India) and of Yunnan (China). From this high region a number of large, elongated river basins run north–south or northwest–southeast. These are the basins of rivers such as the Irrawaddy, Salween, Chao Phraya, Mekong, and Sông Hóng (Red). An east–west traverse across the mainland part of Southeast Asia, therefore, is a repetition of alluvium-filled valleys of large rivers separated by mountain chains or plateaux. To the south and to the east are coastal plains, rocky peninsulas, and a number of deltas. Beyond lies the outer margin of Southeast Asia, the arcuate islands of Indonesia, and the Philippines with steep volcanic slopes, intermontane basins, and flat coastal plains of varying size. This assemblage of landforms has resulted from a combination of plate tectonics, Pleistocene history, Holocene geomorphic processes, and anthropogenic modifications of the landscape. Most of the world has been shaped by such a combination, but unlike the rest of the world, in Southeast Asia all four are important. The conventional wisdom of a primarily climate-driven tropical geomorphology is untenable here. The first two factors, plate tectonics and the Pleistocene history, have been discussed in Chapters 1 and 2 respectively. In the Holocene, Southeast Asia has been affected by the following phenomena: • The sea rose to its present level several thousand years ago. • The present natural vegetation, a major part of which includes a set of rainforest formations, achieved its distribution. • A hot and humid climate became the norm, except in the high altitudes and the extreme northern parts. • The dual monsoon systems blowing from the northeast in the northern hemispheric winter and from the southwest in the summer (and in general producing a large volume of precipitation) became strongly developed.
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Partin, C. A. "A tectonic context for fluctuations in late Paleoproterozoic oxygen content." In Laurentia: Turning Points in the Evolution of a Continent. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.1220(07).

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ABSTRACT Nearly all models of Earth’s oxygenation converge on the premise that the first notable rise of atmospheric oxygen occurred slightly above the Archean-Proterozoic boundary, with the second notable rise occurring just below the Proterozoic-Phanerozoic boundary. Plate tectonic–driven secular changes found above the Archean-Proterozoic boundary are thought to have been partly or wholly responsible for the initial rise in atmospheric O2 in the Great Oxidation Event; however, the role of plate tectonics in oxygen levels thereafter is not well defined. Modern plate tectonics undoubtedly play a role in regulating atmospheric O2 levels. Mountain building, for example, promotes high erosion rates, nutrient delivery to oceans, and efficient biogeochemical cycling of carbon, resulting in the net burial of organic carbon—thought to be the primary regulator of atmospheric O2 levels on geological time scales. The trajectory of atmospheric O2 and oceanic redox conditions in the Proterozoic Eon, representing almost 2 b.y. of geological history, shows a dynamic history with global trends that indicate overall high-low-high O2 levels throughout the Proterozoic Eon, with low-oxygen conditions established by ca. 2.0–1.8 Ga. This contravenes the tenet that major orogenic events (e.g., the Himalaya-scale Trans-Hudson orogen and other coeval orogens that formed the supercontinent Nuna) should yield higher O2 levels, not lower. The contrast of higher O2 early in the Paleoproterozoic with lower O2 later in the Paleoproterozoic is particularly striking, and mechanisms that might have caused this secular change remain unclear. This contribution explores feedbacks related to the tectonic evolution associated with the building of proto-Laurentia and Earth’s first supercontinent, Nuna, and how this impacted the trajectory of atmospheric O2 in the latest Paleoproterozoic Era.
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Kluth, C. F. "Plate Tectonics of the Ancestral Rocky Mountains." In Paleotectonics and sedimentation in the Rocky Mountain Region, United States. American Association of Petroleum Geologists, 1986. http://dx.doi.org/10.1306/m41456c17.

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Chamberlain, C. Page, M. Qasim Jan, and Peter K. Zeitler. "A petrologic record of the collision between the Kohistan Island-Arc and Indian Plate, northwest Himalaya." In Tectonics of the western Himalayas. Geological Society of America, 1989. http://dx.doi.org/10.1130/spe232-p23.

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Hamilton, Warren B. "Driving mechanism and 3-D circulation of plate tectonics." In Special Paper 433: Whence the Mountains? Inquiries into the Evolution of Orogenic Systems: A Volume in Honor of Raymond A. Price. Geological Society of America, 2007. http://dx.doi.org/10.1130/2007.2433(01).

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Gose, Wulf A., Adrián Perarnau, and Jesús Castillo. "Paleomagnetic Results from the Perijá Mountains, VenezuelaAn Example of Vertical Axis Rotation." In The Circum-Gulf of Mexico and the CaribbeanHydrocarbon Habitats, Basin Formation and Plate Tectonics. American Association of Petroleum Geologists, 2003. http://dx.doi.org/10.1306/m79877c44.

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Conference papers on the topic "Plate tectonics – Himalaya Mountains"

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Foley, Daniel J., Paul J. Umhoefer, Paul J. Umhoefer, et al. "REGIONAL SCALE ANCESTRAL ROCKY MOUNTAINS TECTONICS: RELATION TO ASSOCIATED PENNSYLVANIAN–PERMIAN SOUTHEASTERN AND SOUTHWESTERN BASINS AND PLATE MARGINS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-288016.

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Craddock Affinati, Suzanne, Thomas D. Hoisch, Michael L. Wells, and Samuel Wright. "CONSTRAINTS FROM MONAZITE AND XENOTIME PETROCHRONOLOGY ON BURIAL AND EXHUMATION FROM THE FUNERAL MOUNTAINS, CALIFORNIA WITH IMPLICATIONS ON U.S. CORDILLERAN JURASSIC PLATE BOUNDARY TECTONICS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-332760.

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Clark, S. "Regional Tectonics & Structural Framework of Offshore Aceh's Andaman Sub-Basin, Northern Sumatra, Indonesia." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-30.

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The three-way collision of the Indo-Australian, Eurasian and Pacific plates have resulted in Southeast Asia being the most tectonically complex region on Earth. This is particularly true for Offshore Aceh’s Andaman Sub-Basin, which has undergone complex late Eocene-Recent evolution. Despite a long history of hydrocarbon exploration and production, data scarcity in the offshore means that the Sub-Basin’s regional tectonics and structural framework have been poorly understood. Pre-1996 2D seismic data were low-fold and low-offset, however the 2019 PGS (NSMC3D) regional 3D survey imaged the entir
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