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Journal articles on the topic 'Continent-continent collision'

Author: Grafiati

Published: 4 June 2021

Last updated: 3 February 2022

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1

Henyey, T., T. Stern, and P. Molnar. "Continent-continent collision in southern Alps studied." Eos, Transactions American Geophysical Union 74, no. 28 (1993): 316. http://dx.doi.org/10.1029/93eo00454.

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2

Dymkova, Diana, Taras Gerya, and Jean-Pierre Burg. "2D thermomechanical modelling of continent–arc–continent collision." Gondwana Research 32 (April 2016): 138–50. http://dx.doi.org/10.1016/j.gr.2015.02.012.

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3

Shuwen, DONG, WU Hongling, LIU Xiaochun, and XUE Huaimin. "On Continent-Continent Point-Collision and Ultrahigh-Pressure Metamorphism." Acta Geologica Sinica - English Edition 76, no. 1 (2010): 69–80. http://dx.doi.org/10.1111/j.1755-6724.2002.tb00072.x.

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4

Selverstone, Jane, and David S. Gutzler. "Post-125 Ma carbon storage associated with continent-continent collision." Geology 21, no. 10 (1993): 885. http://dx.doi.org/10.1130/0091-7613(1993)021<0885:pmcsaw>2.3.co;2.

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5

Gök, Rengin, Michael E. Pasyanos, and Ekrem Zor. "Lithospheric structure of the continent-continent collision zone: eastern Turkey." Geophysical Journal International 169, no. 3 (2007): 1079–88. http://dx.doi.org/10.1111/j.1365-246x.2006.03288.x.

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6

Brown, D., C. Juhlin, C. Ayala, et al. "Mountain building processes during continent–continent collision in the Uralides." Earth-Science Reviews 89, no. 3-4 (2008): 177–95. http://dx.doi.org/10.1016/j.earscirev.2008.05.001.

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7

Brown, Dennis, Piera Spadea, and Ryo Anma. "Processes of arc–continent collision." Tectonophysics 325, no. 1-2 (2000): vii—viii. http://dx.doi.org/10.1016/s0040-1951(00)00127-x.

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8

Zeng, Rong-sheng, Qing-ju Wu, Zhi-feng Ding, and Lu-pei Zhu. "India-Eurasian collision vs. ocean-continent collision." Acta Seismologica Sinica 20, no. 1 (2007): 1–10. http://dx.doi.org/10.1007/s11589-007-0001-7.

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9

Junwen, CUI, SHI Jinsong, LI Pengwu, ZHANG Xiaowei, GUO Xianpu, and DING Xiaozhong. "Numerical Modeling of Basin-Range Tectonics Related to Continent-Continent Collision." Acta Geologica Sinica - English Edition 79, no. 1 (2005): 24–35. http://dx.doi.org/10.1111/j.1755-6724.2005.tb00864.x.

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10

Uddin, Ashraf, and Neil Lundberg. "Miocene sedimentation and subsidence during continent–continent collision, Bengal basin, Bangladesh." Sedimentary Geology 164, no. 1-2 (2004): 131–46. http://dx.doi.org/10.1016/j.sedgeo.2003.09.004.

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11

Ryan, Paul D. "The role of deep basement during continent-continent collision: a review." Geological Society, London, Special Publications 184, no. 1 (2001): 39–55. http://dx.doi.org/10.1144/gsl.sp.2001.184.01.03.

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12

Verma, R. K. "Gravity field and nature of continent-continent collision along the Himalaya." Physics and Chemistry of the Earth 18 (January 1991): 385–403. http://dx.doi.org/10.1016/0079-1946(91)90011-4.

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13

Caby, Renaud, Uranie Andreopoulos-Renaud, and Christian Pin. "Late Proterozoic arc–continent and continent–continent collision in the pan-African trans-Saharan belt of Mali." Canadian Journal of Earth Sciences 26, no. 6 (1989): 1136–46. http://dx.doi.org/10.1139/e89-097.

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The Tilemsi magmatic arc, preserved along the suture zone of the pan-African trans-Saharan belt of northern Mali, crops out as a series of northeast- to north-northeast-trending strips along the Tilemsi Mesozoic trough and is about 100 km in width. The volcanic arc series includes pillowed metabasalts of tholeiitic character and associated with rhyodacites. Overlying sedimentary rocks are turbiditic volcanic greywackes. They are progressively recrystallized into grey gneiss in the vicinity of gabbro-noritic and dioritic intrusions. U/Pb zircon dating of a crosscutting metaquartz diorite gives

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14

NAGANJANEYULU, K. "Evidence for Continent-Continent Collision Zone in the South Indian Shield Region." Gondwana Research 6, no. 4 (2003): 902–11. http://dx.doi.org/10.1016/s1342-937x(05)71034-0.

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15

Massonne, Hans-Joachim. "Involvement of Crustal Material in Delamination of the Lithosphere after Continent-Continent Collision." International Geology Review 47, no. 8 (2005): 792–804. http://dx.doi.org/10.2747/0020-6814.47.8.792.

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16

White, D. J., M. D. Thomas, A. G. Jones, J. Hope, B. Németh, and Z. Hajnal. "Geophysical transect across a Paleoproterozoic continentcontinent collision zone: The Trans-Hudson Orogen." Canadian Journal of Earth Sciences 42, no. 4 (2005): 385–402. http://dx.doi.org/10.1139/e05-002.

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A summary and comparison of geophysical data and models for the Trans-Hudson Orogen in northern Manitoba and Saskatchewan are presented. Magnetic total field and Bouguer gravity maps are used to define the along-strike extension of geological domains of the orogen exposed on the Canadian Shield, and a two-dimensional density model is produced, which accounts for the observed variations of the Bouguer gravity field across the orogen. An 800-km-long crustal section across the entire continentcontinent collision zone, including the edges of the bounding cratonic blocks, is presented. It incorpor

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17

Kerrick, D., K. Caldeira, J. Selverstone, and D. S. Gutzler. "Post-125 Ma carbon storage associated with continent-continent collision: Comment and Reply." Geology 22, no. 4 (1994): 381–83. http://dx.doi.org/10.1130/0091-7613(1994)022<0381:pmcsaw>2.3.co;2.

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18

Frost, B., C. Frost, S. Swapp, L. Finley-Blasi, and S. Stacey. "Significance of Leucogranitic Gneiss in the Archean Teton Range." UW National Parks Service Research Station Annual Reports 31 (January 1, 2008): 89–92. http://dx.doi.org/10.13001/uwnpsrc.2008.3711.

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In previous years of this project, we have developed the hypothesis that the high-pressure granulites exposed in the Moose Basin area of the Teton Range represent evidence of a 2.7 billion yearÂold continent-continent collision. We have described gneisses in the Teton Range that show two distinct metamorphic histories. In the northwest there are highÂpressure granulites suggesting metamorphism and deformation resulted from a 2685 to 2671 Ma Himalayan type orogeny (Frost et al., 2006). Gneiss exposed in the northwest is dominated by migmatites, with lesser kyanite bearing pelite, and some gar

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19

Brown, D., P. Spadea, V. Puchkov, et al. "Arc–continent collision in the Southern Urals." Earth-Science Reviews 79, no. 3-4 (2006): 261–87. http://dx.doi.org/10.1016/j.earscirev.2006.08.003.

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20

Verma, R. K. "Seismicity of the Himalaya and the northeast India, and nature of continent-continent collision." Physics and Chemistry of the Earth 18 (January 1991): 345–70. http://dx.doi.org/10.1016/0079-1946(91)90009-5.

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21

Sugden, Patrick J., Ivan P. Savov, Samuele Agostini, Marjorie Wilson, Ralf Halama, and Khachatur Meliksetian. "Boron isotope insights into the origin of subduction signatures in continent-continent collision zone volcanism." Earth and Planetary Science Letters 538 (May 2020): 116207. http://dx.doi.org/10.1016/j.epsl.2020.116207.

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22

McGregor, V. R., C. R. L. Friend, and A. P. Nutman. "The late Archaean mobile belt through Godthabsfjord, southern West Greenland: a continent-continent collision zone?" Bulletin of the Geological Society of Denmark 39 (December 20, 1991): 179–97. http://dx.doi.org/10.37570/bgsd-1991-39-08.

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In the Godthabsfjord region of southern West Greenland a NE-SW-trending belt of rocks of very varied age and origin, here named the Akulleq terrane, is separated by major faults from more extensive blocks of typical high-grade Archaean rocks that, although they are superficially similar, have different ages and metamorphic histories. The continental crust that forms the block to the north-west, the Akia terrane, was accreted between ea. 3200 and 2980 Ma, and that forming the block to the south-east, the Tasiusarsuaq terrane, between 2920 and 2800 Ma. It is suggested that the Godthabsfjord belt

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23

DRAUT, AMY E., PETER D. CLIFT, DAVID M. CHEW, MATTHEW J. COOPER, REX N. TAYLOR, and ROBYN E. HANNIGAN. "Laurentian crustal recycling in the Ordovician Grampian Orogeny: Nd isotopic evidence from western Ireland." Geological Magazine 141, no. 2 (2004): 195–207. http://dx.doi.org/10.1017/s001675680400891x.

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Because magmatism associated with subduction is thought to be the principal source for continental crust generation, assessing the relative contribution of pre-existing (subducted and assimilated) continental material to arc magmatism in accreted arcs is important to understanding the origin of continental crust. We present a detailed Nd isotopic stratigraphy for volcanic and volcaniclastic formations from the South Mayo Trough, an accreted oceanic arc exposed in the western Irish Caledonides. These units span an arc–continent collision event, the Grampian (Taconic) Orogeny, in which an intra-

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24

WU, Qingju. "The upper mantle structure of the Tibetan Plateau and its implication for the continent-continent collision." Science in China Series D 48, no. 8 (2005): 1158. http://dx.doi.org/10.1360/03yd0556.

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25

Henrys, S. A., D. J. Woodward, D. Okaya, and J. Yu. "Mapping the Moho beneath the Southern Alps continent-continent collision, New Zealand, using wide-angle reflections." Geophysical Research Letters 31, no. 17 (2004): n/a. http://dx.doi.org/10.1029/2004gl020561.

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26

Hildebrand, P. R., M. P. Searle, Shakirullah, Zafarali Khan, and H. J. Van Heijst. "Geological evolution of the Hindu Kush, NW Frontier Pakistan: active margin to continent-continent collision zone." Geological Society, London, Special Publications 170, no. 1 (2000): 277–93. http://dx.doi.org/10.1144/gsl.sp.2000.170.01.15.

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27

Scarrow, Jane H., Conxi Ayala, and Geoffrey S. Kimbell. "Insights into orogenesis: getting to the root of a continent–ocean–continent collision, Southern Urals, Russia." Journal of the Geological Society 159, no. 6 (2002): 659–71. http://dx.doi.org/10.1144/0016-764901-147.

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28

Zhu, DiCheng, Qing Wang, and ZhiDan Zhao. "Constraining quantitatively the timing and process of continent-continent collision using magmatic record: Method and examples." Science China Earth Sciences 60, no. 6 (2017): 1040–56. http://dx.doi.org/10.1007/s11430-016-9041-x.

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29

Han, Yigui, Guochun Zhao, Peter A. Cawood, Min Sun, Qian Liu, and Jinlong Yao. "Plume-modified collision orogeny: The Tarim–western Tianshan example in Central Asia." Geology 47, no. 10 (2019): 1001–5. http://dx.doi.org/10.1130/g46855.1.

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Abstract Plume-modified orogeny involves the interaction between a mantle plume and subducting oceanic lithosphere at accretionary margins. We propose that a plume can also be involved in collisional orogeny and accounts for the late Paleozoic geological relations in Central Asia. Continental collision between the Tarim and Central Tianshan–Yili blocks at the end Carboniferous resulted in an orogeny lacking continental-type (ultra)high-pressure [(U)HP] rocks and significant syncollision surface erosion and uplift, features normally characteristic of continent-continent interactions. Their abse

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30

Liu, Shaofeng, Ronald Steel, and Guowei Zhang. "Mesozoic sedimentary basin development and tectonic implication, northern Yangtze Block, eastern China: record of continent–continent collision." Journal of Asian Earth Sciences 25, no. 1 (2005): 9–27. http://dx.doi.org/10.1016/j.jseaes.2004.01.010.

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31

Glassley, William E., John A. Korstgård, and Kai Sørensen. "K-rich brine and chemical modification of the crust during continent–continent collision, Nagssugtoqidian Orogen, West Greenland." Precambrian Research 180, no. 1-2 (2010): 47–62. http://dx.doi.org/10.1016/j.precamres.2010.02.020.

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32

Willingshofer, Ernst, J. D. van Wees, S. A. P. L. Cloetingh, and F. Neubauer. "Thermomechanical consequences of Cretaceous continent-continent collision in the eastern Alps (Austria): Insights from two-dimensional modeling." Tectonics 18, no. 5 (1999): 809–26. http://dx.doi.org/10.1029/1999tc900017.

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33

Scheiber, Thomas, O. Adrian Pfiffner, and Guido Schreurs. "Upper crustal deformation in continent-continent collision: A case study from the Bernard nappe complex (Valais, Switzerland)." Tectonics 32, no. 5 (2013): 1320–42. http://dx.doi.org/10.1002/tect.20080.

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34

Tang, J. C., and A. I. Chemenda. "Numerical modelling of arc–continent collision: application to Taiwan." Tectonophysics 325, no. 1-2 (2000): 23–42. http://dx.doi.org/10.1016/s0040-1951(00)00129-3.

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35

Degtyarev, K. E., and A. V. Ryazantsev. "Cambrian arc-continent collision in the Paleozoides of Kazakhstan." Geotectonics 41, no. 1 (2007): 63–86. http://dx.doi.org/10.1134/s0016852107010062.

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36

Lallemand, Serge E., and Char-Shine Liu. "Swath bathymetry reveals active arc-continent collision near Taiwan." Eos, Transactions American Geophysical Union 78, no. 17 (1997): 173. http://dx.doi.org/10.1029/97eo00116.

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37

Charlton, T. R. "Postcollision extension in arc-continent collision zones, eastern Indonesia." Geology 19, no. 1 (1991): 28. http://dx.doi.org/10.1130/0091-7613(1991)019<0028:peiacc>2.3.co;2.

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38

Rangin, C., H. Bellon, F. Benard, J. Letouzey, C. Muller, and T. Sanudin. "Neogene arc-continent collision in Sabah, Northern Borneo (Malaysia)." Tectonophysics 183, no. 1-4 (1990): 305–19. http://dx.doi.org/10.1016/0040-1951(90)90423-6.

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39

Sokolov, S. D., G. Ye Bondarenko, P. W. Layer, and I. R. Kravchenko-Berezhnoy. "South Anyui suture: tectono-stratigraphy, deformations, and principal tectonic events." Stephan Mueller Special Publication Series 4 (September 17, 2009): 201–21. http://dx.doi.org/10.5194/smsps-4-201-2009.

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Abstract. Geochronologic and structural data from the terranes of the South Anyui suture zone record a protracted deformational history before, during and after an Early Cretaceous collision of the passive margin of the Chukotka-Arctic Alaska continental block with the active continental margin of the North Asian continent. Preceding this collision, the island arc complexes of the Yarakvaam terrane on the northern margin of the North Asian craton record Early Carboniferous to Neocomian ages in ophiolite, sedimentary, and volcanic rocks. Triassic to Jurassic amphibolites constrain the timing of

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40

OKAY, ARAL I., İZVER TANSEL, and OKAN TÜYSÜZ. "Obduction, subduction and collision as reflected in the Upper Cretaceous–Lower Eocene sedimentary record of western Turkey." Geological Magazine 138, no. 2 (2001): 117–42. http://dx.doi.org/10.1017/s0016756801005088.

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Late Cretaceous–Early Eocene Tethyan evolution of western Turkey is characterized by ophiolite obduction, high-pressure/low-temperature metamorphism, subduction, arc magmatism and continent–continent collision. The imprints of these events in the Upper Cretaceous–Lower Eocene sedimentary record of western Anatolia are studied in thirty-eight well-described stratigraphic sections. During the Late Cretaceous period, western Turkey consisted of two continents, the Pontides in the north and the Anatolide-Taurides in the south. These continental masses were separated by the İzmir-Ankara Neo-Tethyan

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41

Bunopas, S., P. Vella, H. Fontaine, et al. "Growth of Asia in the Late Triassic Continent-Continent Collision of Shan-Thai and Indochina Against South China." Gondwana Research 4, no. 4 (2001): 584–85. http://dx.doi.org/10.1016/s1342-937x(05)70388-9.

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42

Xia, Yan, Xisheng Xu, Yaoling Niu, and Lei Liu. "Neoproterozoic amalgamation between Yangtze and Cathaysia blocks: The magmatism in various tectonic settings and continent-arc-continent collision." Precambrian Research 309 (May 2018): 56–87. http://dx.doi.org/10.1016/j.precamres.2017.02.020.

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43

Caporali, Alessandro. "Gravimetric constraints on the rheology of the Indian and Tarim Plates in the Karakoram continent–continent collision zone." Journal of Asian Earth Sciences 16, no. 2-3 (1998): 313–21. http://dx.doi.org/10.1016/s0743-9547(98)00005-1.

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44

Liu, XiaoChun, SanZhong Li, and Bor-Ming Jahn. "Tectonic evolution of the Tongbai-Hong’an orogen in central China: From oceanic subduction/accretion to continent-continent collision." Science China Earth Sciences 58, no. 9 (2015): 1477–96. http://dx.doi.org/10.1007/s11430-015-5145-z.

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45

Soloviev, Alexey V., John I. Garver, Mikhail N. Shapiro, Mark T. Brandon, and Jeremy K. Hourigan. "Eocene arc-continent collision in northern Kamchatka, Russian Far East." Russian Journal of Earth Sciences 12, no. 1 (2011): 1–13. http://dx.doi.org/10.2205/2011es000504.

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46

Puchkov, Victor N. "The diachronous (step-wise) arc–continent collision in the Urals." Tectonophysics 479, no. 1-2 (2009): 175–84. http://dx.doi.org/10.1016/j.tecto.2009.01.014.

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47

Nagel, Stefan, Sébastien Castelltort, Andreas Wetzel, Sean D. Willett, Frédéric Mouthereau, and Andrew T. Lin. "Sedimentology and foreland basin paleogeography during Taiwan arc continent collision." Journal of Asian Earth Sciences 62 (January 2013): 180–204. http://dx.doi.org/10.1016/j.jseaes.2012.09.001.

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48

Oncken, O., A. Plesch, J. Weber, W. Ricken, and S. Schrader. "Passive margin detachment during arc-continent collision (Central European Variscides)." Geological Society, London, Special Publications 179, no. 1 (2000): 199–216. http://dx.doi.org/10.1144/gsl.sp.2000.179.01.13.

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49

Bertrand, Edward A., Martyn J. Unsworth, Chih-Wen Chiang, et al. "Magnetotelluric imaging beneath the Taiwan orogen: An arc-continent collision." Journal of Geophysical Research: Solid Earth 117, B1 (2012): n/a. http://dx.doi.org/10.1029/2011jb008688.

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50

LUCAS, S. B., and T. BYRNE. "Footwall involvement during arc-continent collision, Ungava orogen, northern Canada." Journal of the Geological Society 149, no. 2 (1992): 237–48. http://dx.doi.org/10.1144/gsjgs.149.2.0237.

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