Terrane Processes at the Margins of Gondwana: Introduction
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Two Contrasting Phanerozoic Orogenic Systems Revealed by Hafnium Isotope Data William J
ARTICLES PUBLISHED ONLINE: 17 APRIL 2011 | DOI: 10.1038/NGEO1127 Two contrasting Phanerozoic orogenic systems revealed by hafnium isotope data William J. Collins1*(, Elena A. Belousova2, Anthony I. S. Kemp1 and J. Brendan Murphy3 Two fundamentally different orogenic systems have existed on Earth throughout the Phanerozoic. Circum-Pacific accretionary orogens are the external orogenic system formed around the Pacific rim, where oceanic lithosphere semicontinuously subducts beneath continental lithosphere. In contrast, the internal orogenic system is found in Europe and Asia as the collage of collisional mountain belts, formed during the collision between continental crustal fragments. External orogenic systems form at the boundary of large underlying mantle convection cells, whereas internal orogens form within one supercell. Here we present a compilation of hafnium isotope data from zircon minerals collected from orogens worldwide. We find that the range of hafnium isotope signatures for the external orogenic system narrows and trends towards more radiogenic compositions since 550 Myr ago. By contrast, the range of signatures from the internal orogenic system broadens since 550 Myr ago. We suggest that for the external system, the lower crust and lithospheric mantle beneath the overriding continent is removed during subduction and replaced by newly formed crust, which generates the radiogenic hafnium signature when remelted. For the internal orogenic system, the lower crust and lithospheric mantle is instead eventually replaced by more continental lithosphere from a collided continental fragment. Our suggested model provides a simple basis for unravelling the global geodynamic evolution of the ancient Earth. resent-day orogens of contrasting character can be reduced to which probably began by the Early Ordovician12, and the Early two types on Earth, dominantly accretionary or dominantly Paleozoic accretionary orogens in the easternmost Altaids of Pcollisional, because only the latter are associated with Wilson Asia13. -
Subduction Polarity in Ancient Arcs: a Call to Integrate Geology And
COMMENT & REPLY Subduction Polarity in Ancient Arcs: A Call to Integrate Geology and Geophysics to Decipher the Mesozoic Tectonic History of the Northern Cordillera of North America: REPLY Terry L. Pavlis, Dept. of Geological Sciences, University of Texas, El Paso, Texas 79968, USA; Jeffrey M. Amato, Dept. of Geological Sciences, New Mexico State University, Las Cruces, New Mexico 88003, USA; Jeffrey M. Trop, Dept. of Geology and Environmental Geosciences, Bucknell University, Lewisburg, Pennsylvania 17837, USA; Kenneth D. Ridgway, Dept. of Earth, Atmospheric and Planetary Sciences, Purdue University, West Lafayette, Indiana 47907, USA; Sarah M. Roeske, Earth and Planetary Sciences Dept., University of California, Davis, California 95616, USA; and George E. Gehrels, Dept. of Geosciences, University of Arizona, Tucson, Arizona, 85721, USA INTRODUCTION drafts of the paper. However, when we problem is not solved, which underscores We welcome the opportunity to discuss the realized that experts in this field were our conclusion that resolving ancient sub- views expressed by Sigloch and Mihalynuk in actively debating the topic, we reduced our duction polarity problems requires a con- their Comment (Sigloch and Mihalynuk, discussion to a short paragraph. In their certed collaborative effort between the geo- 2020; referred to here as SM) on Pavlis et al. Comment, SM reiterate parts of their model logic and geophysical communities. (2019) because it provides an opportunity to but emphasize a consensus in the geophysi- A foundation of Sigloch and Mihalynuk’s elaborate on the criteria for determining sub- cal community that deep mantle tomo- (2013, 2017) interpretations is that plate duction polarity, an important problem in the graphic anomalies are subduction zone rem- reconstructions restore North America to a North American Cordillera and for tectonic nants. -
(Ordovícico) En El Segmento Andino Central Del Orógeno Terra Australis
XII Congreso Geológico Chileno Santiago, 22-26 Noviembre, 2009 S9_011 La tectónica acrecional oclóyica (Ordovícico) en el segmento andino central del orógeno Terra Australis Astini R.A.1, Martina F.1 1Laboratorio de Análisis de Cuencas, CICTERRA-Universidad Nacional de Córdoba, Av. Velez Sarsfield 1611, 2º piso, of. 7, X5016GCA Córdoba, Argentina. [email protected] En el marco del orógeno acrecional de Terra Australis [1] se reconocen intervalos temporales con acreción de terrenos e interrupción momentánea de la subducción que afectan diferencialmente al margen protoandino y permiten reconocer segmentos con características e historias contrastadas en los Andes. Sobre la base de una revisión conceptual y bibliográfica y de nuevos estudios estratigráficos, geoquímicos e isotópicos en la región del antepaís andino central se propone un mecanismo acrecional alternativo para la etapa de orogénesis ordovícica, que es la de mayor extensión que haya afectado al margen proto-pacífico antes de la orogenia gondwánica, con que finaliza la historia acrecional paleozoica. Dentro de la etapa de orogénesis oclóyica se propone separar la colisión del terreno de Precordillera [2] en el segmento andino central entre 27°30’ y 36°30’ LS aproximadamente (~1000 km de longitud), de la acreción de un bloque alargado (sliver o ribbon terrane) de basamento mesoproterozoico de mucho mayor extensión longitudinal (superior los 2000 km) (Fig. 1) que, de alguna manera, ha sido denominado Occidentalia [3]. Este último incluiría en los Andes Centrales a los terrenos de basamento mesoproterozoico correspondientes a las Sierras Pampeanas Occidentales, ubicados al oeste del cinturón de Famatina y su continuación septentrional en la Puna Catamarqueña (afloramientos de Casadero Grande) y en los terrenos de Arequipa-Antofalla. -
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R. J. PANKHURST (CHIEF EDITOR) P. DOYLE E J. GREGORY J. S. GRIFFITHS A. J. HARTLEY R. E. HOLDSWORTH A. C. MORTON N. S. ROBINS M. S. STOKER J. P. TURNER Special Publication reviewing procedures The Society makes every effort to ensure that the scientific and production quality of its books matches that of its journals. Since 1997, all book proposals have been refereed by specialist reviewers as well as by the Society's Books Editorial Committee. If the referees identify weaknesses in the proposal, these must be addressed before the proposal is accepted. Once the book is accepted, the Society has a team of Book Editors (listed above) who ensure that the volume editors follow strict guidelines on refereeing and quality control. We insist that individual papers can only be accepted after satis- factory review by two independent referees. The questions on the review forms are similar to those for Journal of the Geological Society. The referees' forms and comments must be available to the Society's Book Editors on request. Although many of the books result from meetings, the editors are expected to commission papers that were not pre- sented at the meeting to ensure that the book provides a balanced coverage of the subject. Being accepted for presentation at the meeting does not guarantee inclusion in the book. Geological Society Special Publications are included in the ISI Science Citation Index, but they do not have an impact factor, the latter being applicable only to journals. -
Back Matter (PDF)
Index Page numbers in italic refer to tables, and those in bold to figures. accretionary orogens, defined 23 Namaqua-Natal Orogen 435-8 Africa, East SW Angola and NW Botswana 442 Congo-Sat Francisco Craton 4, 5, 35, 45-6, 49, 64 Umkondo Igneous Province 438-9 palaeomagnetic poles at 1100-700 Ma 37 Pan-African orogenic belts (650-450 Ma) 442-50 East African(-Antarctic) Orogen Damara-Lufilian Arc-Zambezi Belt 3, 435, accretion and deformation, Arabian-Nubian Shield 442-50 (ANS) 327-61 Katangan basaltic rocks 443,446 continuation of East Antarctic Orogen 263 Mwembeshi Shear Zone 442 E/W Gondwana suture 263-5 Neoproterozoic basin evolution and seafloor evolution 357-8 spreading 445-6 extensional collapse in DML 271-87 orogenesis 446-51 deformations 283-5 Ubendian and Kibaran Belts 445 Heimefront Shear Zone, DML 208,251, 252-3, within-plate magmatism and basin initiation 443-5 284, 415,417 Zambezi Belt 27,415 structural section, Neoproterozoic deformation, Zambezi Orogen 3, 5 Madagascar 365-72 Zambezi-Damara Belt 65, 67, 442-50 see also Arabian-Nubian Shield (ANS); Zimbabwe Belt, ophiolites 27 Mozambique Belt Zimbabwe Craton 427,433 Mozambique Belt evolution 60-1,291, 401-25 Zimbabwe-Kapvaal-Grunehogna Craton 42, 208, 250, carbonates 405.6 272-3 Dronning Mand Land 62-3 see also Pan-African eclogites and ophiolites 406-7 Africa, West 40-1 isotopic data Amazonia-Rio de la Plata megacraton 2-3, 40-1 crystallization and metamorphic ages 407-11 Birimian Orogen 24 Sm-Nd (T DM) 411-14 A1-Jifn Basin see Najd Fault System lithologies 402-7 Albany-Fraser-Wilkes -
Billion Year Cyclicity Through Earth History: Causes and Consequences
Geophysical Research Abstracts Vol. 21, EGU2019-12040, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. Billion year cyclicity through Earth history: causes and consequences William Collins (1), Erin Martin (1), Ross Mitchell (1), Brendan Murphy (2), and Chris Spencer (1) (1) Curtin University, School of Earth & Planetary Sciences, Perth, Australia ([email protected]), (2) St. Francis Xavier University, Department of Earth Sciences, Antigonish, NS, B2G 2W5, Canada A billion year-scale (gigacycle) periodicity in global radiogenic Hf and Sr isotopic trends is investigated by integrating data from tectonics, geodynamics, and palaeomagnetism, in order to build a holistic geodynamic model linking modes of mantle convection to plate tectonic motions over the last 2,500 Myr. The gigacycle reflects an alternating dominance between degree-2 and degree-1 mantle convective flow, manifest as the presence or absence of a hemispheric subduction girdle, respectively. Degree-1 convection involves a single upwelling and opposed downwelling zone, whereas degree-2 has two upwelling zones located antipodally. Present-day convection is degree-2, with the two modern upwelling zones as the Pacific and African superplumes, located on either side of the circum-Pacific subduction girdle. The girdle is geologically recorded by circum-Pacific accretionary orogens, and has existed since ∼550 Myr, indicating that degree-2 convection characterises the Phanerozoic eon. Degree-1 convection resulted in the amalgamation of Columbia ca. 2,000 Myr ago and Gondwana ca. 550 Myr ago accompanied by peaks in crustal reworking (-"Hf), whereas degree-2 convection produced Nuna ca. 1,600 Myr ago and Pangaea 200 Myr ago accompanied by peaks in mantle input (+"Hf). -
Paleomagnetic and Geochronological Studies of the Mafic Dyke Swarms Of
Precambrian Research 198–199 (2012) 51–76 Contents lists available at SciVerse ScienceDirect Precambrian Research journa l homepage: www.elsevier.com/locate/precamres Paleomagnetic and geochronological studies of the mafic dyke swarms of Bundelkhand craton, central India: Implications for the tectonic evolution and paleogeographic reconstructions a,∗ a b a c Vimal R. Pradhan , Joseph G. Meert , Manoj K. Pandit , George Kamenov , Md. Erfan Ali Mondal a Department of Geological Sciences, University of Florida, 241 Williamson Hall, Gainesville, FL 32611, USA b Department of Geology, University of Rajasthan, Jaipur 302004, Rajasthan, India c Department of Geology, Aligarh Muslim University, Aligarh 202002, India a r t i c l e i n f o a b s t r a c t Article history: The paleogeographic position of India within the Paleoproterozoic Columbia and Mesoproterozoic Received 12 July 2011 Rodinia supercontinents is shrouded in uncertainty due to the paucity of high quality paleomagnetic Received in revised form 6 November 2011 data with strong age control. New paleomagnetic and geochronological data from the Precambrian mafic Accepted 18 November 2011 dykes intruding granitoids and supracrustals of the Archean Bundelkhand craton (BC) in northern Penin- Available online 28 November 2011 sular India is significant in constraining the position of India at 2.0 and 1.1 Ga. The dykes are ubiquitous within the craton and have variable orientations (NW–SE, NE–SW, ENE–WSW and E–W). Three dis- Keywords: tinct episodes of dyke intrusion are inferred from the paleomagnetic analysis of these dykes. The older Bundelkhand craton, Mafic dykes, Central ◦ NW–SE trending dykes yield a mean paleomagnetic direction with a declination = 155.3 and an incli- India, Paleomagnetism, Geochronology, ◦ ◦ − Ä ˛ Paleogeography nation = 7.8 ( = 21; 95 = 9.6 ). -
New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island Area and Brooks Range, Alaska
Geologica Acta, Vol.12, Nº 1, March 2014, 29-52 DOI: 10.1344/105.000002074 New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island area and Brooks Range, Alaska J. FEDOROWSKI1 C.H. STEVENS2 E. KATVALA3 1Institute of Geology, Adam Mickiewicz University Makow Polnych 16, PL-61-606, Poznan, Poland. E-mail: [email protected] 2Department of Geology, San Jose Unversity San Jose, California 95192, USA. E-mail: [email protected] 3Department of Geology, University of Calgary Calgary, Canada. E-mail: [email protected] ABS TRACT Three new species of the genus Heritschioides, i.e., H. alaskensis sp. nov., H. kuiuensis sp. nov., and H. splendidus sp. nov., and Kekuphyllum sandoense gen. et sp. nov. from the northeastern Kuiu Island area and nearby islets, part of Alexander terrane in southeastern Alaska, and Heritschioides separatus sp. nov. from the Brooks Range, Alaska, are described and illustrated. The three new fasciculate colonial coral species from the Kuiu Island area, collected from the Moscovian Saginaw Bay Formation, are phylogenetically related to those of probable Bashkirian age in the Brooks Range in northern Alaska as shown by the presence of morphologically similar species of Heritschioides. These corals from both areas also are related to one species in the Quesnel terrane in western Canada. Kekuphyllum sandoense from the Saginaw Bay Formation of the Kuiu Island area is the only cerioid-aphroid species within the Subfamily Heritschioidinae described so far. The complete early ontogeny of a protocorallite is for the first time described here on a basis of H. kuiuensis sp. nov. and compared to the hystero-ontogeny in order to show similarities and differences in those processes. -
Locating South China in Rodinia and Gondwana: a Fragment of Greater India Lithosphere?
Locating South China in Rodinia and Gondwana: A fragment of greater India lithosphere? Peter A. Cawood1, 2, Yuejun Wang3, Yajun Xu4, and Guochun Zhao5 1Department of Earth Sciences, University of St Andrews, North Street, St Andrews KY16 9AL, UK 2Centre for Exploration Targeting, School of Earth and Environment, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia 3State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China 4State Key Laboratory of Biogeology and Environmental Geology, Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China 5Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong, China ABSTRACT metamorphosed Neoproterozoic strata and From the formation of Rodinia at the end of the Mesoproterozoic to the commencement unmetamorphosed Sinian cover (Fig. 1; Zhao of Pangea breakup at the end of the Paleozoic, the South China craton fi rst formed and then and Cawood, 2012). The Cathaysia block is com- occupied a position adjacent to Western Australia and northern India. Early Neoproterozoic posed predominantly of Neoproterozoic meta- suprasubduction zone magmatic arc-backarc assemblages in the craton range in age from ca. morphic rocks, with minor Paleoproterozoic and 1000 Ma to 820 Ma and display a sequential northwest decrease in age. These relations sug- Mesoproterozoic lithologies. Archean basement gest formation and closure of arc systems through southeast-directed subduction, resulting is poorly exposed and largely inferred from the in progressive northwestward accretion onto the periphery of an already assembled Rodinia. presence of minor inherited and/or xenocrys- Siliciclastic units within an early Paleozoic succession that transgresses across the craton were tic zircons in younger rocks (Fig. -
Wrangellia Flood Basalts in Alaska, Yukon, and British Columbia: Exploring the Growth and Magmatic History of a Late Triassic Oceanic Plateau
WRANGELLIA FLOOD BASALTS IN ALASKA, YUKON, AND BRITISH COLUMBIA: EXPLORING THE GROWTH AND MAGMATIC HISTORY OF A LATE TRIASSIC OCEANIC PLATEAU By ANDREW R. GREENE A THESIS SUBMITTED iN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES (Geological Sciences) UNIVERSITY OF BRITISH COLUMBIA (Vancouver) August 2008 ©Andrew R. Greene, 2008 ABSTRACT The Wrangellia flood basalts are parts of an oceanic plateau that formed in the eastern Panthalassic Ocean (ca. 230-225 Ma). The volcanic stratigraphy presently extends >2300 km in British Columbia, Yukon, and Alaska. The field relationships, age, and geochemistry have been examined to provide constraints on the construction of oceanic plateaus, duration of volcanism, source of magmas, and the conditions of melting and magmatic evolution for the volcanic stratigraphy. Wrangellia basalts on Vancouver Island (Karmutsen Formation) form an emergent sequence consisting of basal sills, submarine flows (>3 km), pillow breccia and hyaloclastite (<1 1cm), and subaerial flows (>1.5 km). Karmutsen stratigraphy overlies Devonian to Permian volcanic arc (—‘380-355 Ma) and sedimentary sequences and is overlain by Late Triassic limestone. The Karmutsen basalts are predominantly homogeneous tholeiitic basalt (6-8 wt% MgO); however, the submarine part of the stratigraphy, on northern Vancouver Island, contains picritic pillow basalts (9-20 wt% MgO). Both lava groups have overlapping initial and ENd, indicating a common, ocean island basalt (OIB)-type Pacific mantle source similar to the source of basalts from the Ontong Java and Caribbean Plateaus. The major-element chemistry of picrites indicates extensive melting (23 -27%) of anomalously hot mantle (‘—1500°C), which is consistent with an origin from a mantle plume head. -
Pan-African Orogeny 1
Encyclopedia 0f Geology (2004), vol. 1, Elsevier, Amsterdam AFRICA/Pan-African Orogeny 1 Contents Pan-African Orogeny North African Phanerozoic Rift Valley Within the Pan-African domains, two broad types of Pan-African Orogeny orogenic or mobile belts can be distinguished. One type consists predominantly of Neoproterozoic supracrustal and magmatic assemblages, many of juvenile (mantle- A Kröner, Universität Mainz, Mainz, Germany R J Stern, University of Texas-Dallas, Richardson derived) origin, with structural and metamorphic his- TX, USA tories that are similar to those in Phanerozoic collision and accretion belts. These belts expose upper to middle O 2005, Elsevier Ltd. All Rights Reserved. crustal levels and contain diagnostic features such as ophiolites, subduction- or collision-related granitoids, lntroduction island-arc or passive continental margin assemblages as well as exotic terranes that permit reconstruction of The term 'Pan-African' was coined by WQ Kennedy in their evolution in Phanerozoic-style plate tectonic scen- 1964 on the basis of an assessment of available Rb-Sr arios. Such belts include the Arabian-Nubian shield of and K-Ar ages in Africa. The Pan-African was inter- Arabia and north-east Africa (Figure 2), the Damara- preted as a tectono-thermal event, some 500 Ma ago, Kaoko-Gariep Belt and Lufilian Arc of south-central during which a number of mobile belts formed, sur- and south-western Africa, the West Congo Belt of rounding older cratons. The concept was then extended Angola and Congo Republic, the Trans-Sahara Belt of to the Gondwana continents (Figure 1) although West Africa, and the Rokelide and Mauretanian belts regional names were proposed such as Brasiliano along the western Part of the West African Craton for South America, Adelaidean for Australia, and (Figure 1). -
Destruction of the North China Craton
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/257684968 Destruction of the North China Craton Article in Science China Earth Science · October 2012 Impact Factor: 1.49 · DOI: 10.1007/s11430-012-4516-y CITATIONS READS 69 65 6 authors, including: Rixiang Zhu Yi-Gang Xu Chinese Academy of Sciences Chinese Academy of Sciences 264 PUBLICATIONS 8,148 CITATIONS 209 PUBLICATIONS 7,351 CITATIONS SEE PROFILE SEE PROFILE Tianyu Zheng Chinese Academy of Sciences 62 PUBLICATIONS 1,589 CITATIONS SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: Yi-Gang Xu letting you access and read them immediately. Retrieved on: 26 May 2016 SCIENCE CHINA Earth Sciences Progress of Projects Supported by NSFC October 2012 Vol.55 No.10: 1565–1587 • REVIEW • doi: 10.1007/s11430-012-4516-y Destruction of the North China Craton ZHU RiXiang1*, XU YiGang2, ZHU Guang3, ZHANG HongFu1, XIA QunKe4 & ZHENG TianYu1 1 State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2 State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 3 School of Resource and Environmental Engineering, Hefei University of Technology, Hefei 230009, China; 4 School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China Received March 27, 2012; accepted June 18, 2012 A National Science Foundation of China (NSFC) major research project, Destruction of the North China Craton (NCC), has been carried out in the past few years by Chinese scientists through an in-depth and systematic observations, experiments and theoretical analyses, with an emphasis on the spatio-temporal distribution of the NCC destruction, the structure of deep earth and shallow geological records of the craton evolution, the mechanism and dynamics of the craton destruction.