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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. -
Brooklyn College and Graduate School of the City University of NY, Brooklyn, NY 11210 and Northeastern Science Foundation Affiliated with Brooklyn College, CUNY, P.O
FLYSCH AND MOLASSE OF THE CLASSICAL TACONIC AND ACADIAN OROGENIES: MODELS FOR SUBSURFACE RESERVOIR SETTINGS GERALD M. FRIEDMAN Brooklyn College and Graduate School of the City University of NY, Brooklyn, NY 11210 and Northeastern Science Foundation affiliated with Brooklyn College, CUNY, P.O. Box 746, Troy, NY 12181 ABSTRACT This field trip will examine classical sections of the Appalachians including Cambro-Ordovician basin-margin and basin-slope facies (flysch) of the Taconics and braided and meandering stteam deposits (molasse) of the Catskills. The deep water settings are part of the Taconic sequence. These rocks include massive sandstones of excellent reservoir quality that serve as models for oil and gas exploration. With their feet, participants may straddle the classical Logan's (or Emmon 's) line thrust plane. The stream deposits are :Middle to Upper Devonian rocks of the Catskill Mountains which resulted from the Acadian Orogeny, where the world's oldest and largest freshwater clams can be found in the world's oldest back-swamp fluvial facies. These fluvial deposits make excellent models for comparable subsurface reservoir settings. INTRODUCTION This trip will be in two parts: (1) a field study of deep-water facies (flysch) of the Taconics, and (2) a field study of braided- and meandering-stream deposits (molasse) of the Catskills. The rocks of the Taconics have been debated for more than 150 years and need to be explained in detail before the field stops make sense to the uninitiated. Therefore several pages of background on these deposits precede the itinera.ry. The Catskills, however, do not need this kind of orientation, hence after the Taconics (flysch) itinerary, the field stops for the Catskills follow immediately without an insertion of background informa tion. -
Neoproterozoic Glaciations in a Revised Global Palaeogeography from the Breakup of Rodinia to the Assembly of Gondwanaland
Sedimentary Geology 294 (2013) 219–232 Contents lists available at SciVerse ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Invited review Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland Zheng-Xiang Li a,b,⁎, David A.D. Evans b, Galen P. Halverson c,d a ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, GPO Box U1987, Perth, WA 6845, Australia b Department of Geology and Geophysics, Yale University, New Haven, CT 06520-8109, USA c Earth & Planetary Sciences/GEOTOP, McGill University, 3450 University St., Montreal, Quebec H3A0E8, Canada d Tectonics, Resources and Exploration (TRaX), School of Earth and Environmental Sciences, University of Adelaide, SA 5005, Australia article info abstract Article history: This review paper presents a set of revised global palaeogeographic maps for the 825–540 Ma interval using Received 6 January 2013 the latest palaeomagnetic data, along with lithological information for Neoproterozoic sedimentary basins. Received in revised form 24 May 2013 These maps form the basis for an examination of the relationships between known glacial deposits, Accepted 28 May 2013 palaeolatitude, positions of continental rifting, relative sea-level changes, and major global tectonic events Available online 5 June 2013 such as supercontinent assembly, breakup and superplume events. This analysis reveals several fundamental ’ Editor: J. Knight palaeogeographic features that will help inform and constrain models for Earth s climatic and geodynamic evolution during the Neoproterozoic. First, glacial deposits at or near sea level appear to extend from high Keywords: latitudes into the deep tropics for all three Neoproterozoic ice ages (Sturtian, Marinoan and Gaskiers), al- Neoproterozoic though the Gaskiers interval remains very poorly constrained in both palaeomagnetic data and global Rodinia lithostratigraphic correlations. -
Balkatach Hypothesis: a New Model for the Evolution of the Pacific, Tethyan, and Paleo-Asian Oceanic Domains
Research Paper GEOSPHERE Balkatach hypothesis: A new model for the evolution of the Pacific, Tethyan, and Paleo-Asian oceanic domains 1,2 2 GEOSPHERE, v. 13, no. 5 Andrew V. Zuza and An Yin 1Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 2Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, California 90095-1567, USA doi:10.1130/GES01463.1 18 figures; 2 tables; 1 supplemental file ABSTRACT suturing. (5) The closure of the Paleo-Asian Ocean in the early Permian was accompanied by a widespread magmatic flare up, which may have been CORRESPONDENCE: avz5818@gmail .com; The Phanerozoic history of the Paleo-Asian, Tethyan, and Pacific oceanic related to the avalanche of the subducted oceanic slabs of the Paleo-Asian azuza@unr .edu domains is important for unraveling the tectonic evolution of the Eurasian Ocean across the 660 km phase boundary in the mantle. (6) The closure of the and Laurentian continents. The validity of existing models that account for Paleo-Tethys against the southern margin of Balkatach proceeded diachro- CITATION: Zuza, A.V., and Yin, A., 2017, Balkatach hypothesis: A new model for the evolution of the the development and closure of the Paleo-Asian and Tethyan Oceans criti- nously, from west to east, in the Triassic–Jurassic. Pacific, Tethyan, and Paleo-Asian oceanic domains: cally depends on the assumed initial configuration and relative positions of Geosphere, v. 13, no. 5, p. 1664–1712, doi:10.1130 the Precambrian cratons that separate the two oceanic domains, including /GES01463.1. the North China, Tarim, Karakum, Turan, and southern Baltica cratons. -
The Eighth Continent?
www.Breaking News English.com Ready-to-Use English Lessons by Sean Banville “1,000 IDEAS & ACTIVITIES Thousands more free lessons FOR LANGUAGE TEACHERS” from Sean's other websites www.breakingnewsenglish.com/book.html www.freeeslmaterials.com/sean_banville_lessons.html Level 2 Zealandia – The eighth continent? 19th February, 2017 http://www.breakingnewsenglish.com/1702/170219-zealandia-2.html Contents The Reading 2 Phrase Matching 3 Listening Gap Fill 4 No Spaces 5 Survey 6 Writing and Speaking 7 Writing 8 Please try Levels 0, 1 and 3. They are (a little) harder. Twitter twitter.com/SeanBanville Facebook www.facebook.com/pages/BreakingNewsEnglish/155625444452176 Google + https://plus.google.com/+SeanBanville THE READING From http://www.breakingnewsenglish.com/1702/170219-zealandia-2.html We used to believe there were nine planets, but now there are eight (Pluto is not a planet). Now we may have to change how many continents there are. We are taught there are seven - Asia, Africa, North and South America, Antarctica, Europe, and Australia. Geologists now say there is an eighth continent - Zealandia. This is a big, largely underwater landmass in the Pacific Ocean. Six per cent of it is above water and is New Zealand and New Caledonia. The rest is under the ocean. It is five million square kilometres, which scientists say is big enough to be a continent. Geologists explained why Zealandia is a continent in a research paper in the Geological Society of America's Journal. They argue that the land does not have to be above water to be a continent. They said Zealandia is a continent because of four points: It is a lot higher than the area around it, it has a special geology, it is easy to see its shape, and it is thicker than the ocean floor. -
Kinematics and Extent of the Piemont-Liguria Basin
https://doi.org/10.5194/se-2020-161 Preprint. Discussion started: 8 October 2020 c Author(s) 2020. CC BY 4.0 License. Kinematics and extent of the Piemont-Liguria Basin – implications for subduction processes in the Alps Eline Le Breton1, Sascha Brune2,3, Kamil Ustaszewski4, Sabin Zahirovic5, Maria Seton5, R. Dietmar Müller5 5 1Department of Earth Sciences, Freie Universität Berlin, Germany 2Geodynamic Modelling Section, German Research Centre for Geosciences, GFZ Potsdam, Germany 3Institute of Geosciences, University of Potsdam, Potsdam, Germany 4Institute for Geological Sciences, Friedrich-Schiller-Universität Jena, Germany 10 5EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia Correspondence to: Eline Le Breton ([email protected]) Abstract. Assessing the size of a former ocean, of which only remnants are found in mountain belts, is challenging but crucial to understand subduction and exhumation processes. Here we present new constraints on the opening and width of the Piemont- Liguria (PL) Ocean, known as the Alpine Tethys together with the Valais Basin. We use a regional tectonic reconstruction of 15 the Western Mediterranean-Alpine area, implemented into a global plate motion model with lithospheric deformation, and 2D thermo-mechanical modelling of the rifting phase to test our kinematic reconstructions for geodynamic consistency. Our model fits well with independent datasets (i.e. ages of syn-rift sediments, rift-related fault activity and mafic rocks) and shows that the PL Basin opened in four stages: (1) Rifting of the proximal continental margin in Early Jurassic (200-180 Ma), (2) Hyper- extension of the distal margin in Early-Middle Jurassic (180-165 Ma), (3) Ocean-Continent Transition (OCT) formation with 20 mantle exhumation and MORB-type magmatism in Middle-Late Jurassic (165-154 Ma), (4) Break-up and “mature” oceanic spreading mostly in Late Jurassic (154-145 Ma). -
Redalyc.Lost Terranes of Zealandia: Possible Development of Late
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Adams, Christopher J Lost Terranes of Zealandia: possible development of late Paleozoic and early Mesozoic sedimentary basins at the southwest Pacific margin of Gondwanaland, and their destination as terranes in southern South America Andean Geology, vol. 37, núm. 2, julio, 2010, pp. 442-454 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173916371010 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Ge%gy 37 (2): 442-454. July. 2010 Andean Geology formerly Revista Geológica de Chile www.scielo.cl/andgeol.htm Lost Terranes of Zealandia: possible development of late Paleozoic and early Mesozoic sedimentary basins at the southwest Pacific margin of Gondwana land, and their destination as terranes in southern South America Christopher J. Adams GNS Science, Private Bag 1930, Dunedin, New Zealand. [email protected] ABSTRACT. Latesl Precambrian to Ordovician metasedimentary suecessions and Cambrian-Ordovician and Devonian Carboniferous granitoids form tbe major par! oftbe basemenl of soutbem Zealandia and adjacenl sectors ofAntarctica and southeastAustralia. Uplift/cooling ages ofthese rocks, and local Devonian shallow-water caver sequences suggest tbal final consolidation oftbe basemenl occurred tbrough Late Paleozoic time. A necessary consequence oftlris process would have been contemporaneous erosion and tbe substantial developmenl of marine sedimentary basins al tbe Pacific margin of Zealandia. -
Gondwana Large Igneous Provinces (Lips): Distribution, Diversity and Significance
Downloaded from http://sp.lyellcollection.org/ by guest on September 30, 2021 Gondwana Large Igneous Provinces (LIPs): distribution, diversity and significance SARAJIT SENSARMA1*, BRYAN C. STOREY2 & VIVEK P. MALVIYA3 1Centre of Advanced Study in Geology, University of Lucknow, Lucknow, Uttar Pradesh 226007, India 2Gateway Antarctica, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand 324E Mayur Residency Extension, Faridi Nagar, Lucknow, Uttar Pradesh 226016, India *Correspondence: [email protected] Abstract: Gondwana, comprising >64% of the present-day continental mass, is home to 33% of Large Igneous Provinces (LIPs) and is key to unravelling the lithosphere–atmosphere system and related tectonics that mediated global climate shifts and sediment production conducive for life on Earth. Increased recognition of bimodal LIPs in Gondwana with significant, sometimes subequal, proportions of synchronous silicic volcanic rocks, mostly rhyolites to high silica rhyolites (±associ- ated granitoids) to mafic volcanic rocks is a major frontier, not considered in mantle plume or plate process hypotheses. On a δ18O v. initial 87Sr/86Sr plot for silicic rocks in Gondwana LIPs there is a remarkable spread between continental crust and mantle values, signifying variable contributions of crust and mantle in their origins. Caldera-forming silicic LIP events were as large as their mafic counterparts, and erupted for a longer duration (>20 myr). Several Gondwana LIPs erupted near the active continental margins, in addition to within-continents; rifting, however, continued even after LIP emplacements in several cases or was aborted and did not open into ocean by coeval com- pression. Gondwana LIPs had devastating consequences in global climate shifts and are major global sediment sources influencing upper continental crust compositions. -
IGA News No. 92
IGA NEWS Newsletter of the International Geothermal Association Quarterly No. 109 1 IGA ACTIVITIES CONTENTS IGA ACTIVITIES Message from the Executive Message from the Executive Director... 1 Director 41st GRC Annual Meeting… 2 Greetings to all members of the IGA and to those that 2nd Annual General Assembly of GEMex Project… 3 are reading this newsletter. As mentioned in our MEXIREC 2017 and REN21 SC Meeting… 5 previous writing, the IGA Board has developed a new strategy which will help us to strengthen the role of our AFRICA members and the wider geothermal energy community Djibouti: Kuwaiti Grant for Geothermal Program… 7 not only for our sector, but also in the wider context of Ethiopia: Japanese Grant, and Geothermal Projects … 7 the ongoing renewable energy and climate change Kenya: Several Geothermal Notes… 9 debate. Tanzania: CIF to Fund the Ngozi Project: … 11 The IGA has been very busy over the past months to AMERICAS initiate strategic activities aligned with our four Pillars: Chile: Two Notes… 12 &13 Visibility, Authority, Independence and Costa Rica: Miravalles Renamed, Loan at Risk… 14 Membership. In this newsletter I focus on Pillar Ecuador: Exploration at the Chachimbiro Project … 15 Visibility: it is with great pride that I can show you our Honduras: First Geothermal Plant in Operation… 15 new logo and visual identity for the IGA (see the right Latin America: 8 Projects to Be Granted by GDF… 16 upper part of this page). We thank Team Visibility Mexico: Old Well Flows & Portable Plant… 17 (Andy Blair, Jane Brotheridge, Kristin Vala United States: Several Notes… 18 Matthiasdottir, and Bjarni Bjarnasson) for their great ASIA / PACIFIC RIM work and support. -
North America Free Download
NORTH AMERICA FREE DOWNLOAD Libby Koponen | 48 pages | 01 Mar 2009 | Children's Press(CT) | 9780531218303 | English | New York, NY, United States North America Plymouth remains the de jure capital. With soldiers in tow, his goal was to find gold for the Spanish Crown. United States of America Bureau of the Census. Nearly North America million immigrants have a four-year college degree or better. Retrieved 3 October This North America a list of North American countries and dependent territories by population. New Spain, a territory that stretched from the southwestern modern-day U. He explained the rationale for the name in the accompanying book Cosmographiae Introductio : [6]. This section needs expansion. Oceans portal Book Category. About ten years later another trading company, the West India Company, settled groups of colonists on Manhattan Island and at Fort Orange. North America has been historically referred to by other names. The first attempt by Europeans to colonize the New World occurred around A. Weishampel, David B. Demographics by North America. Other French-speaking locales include the Province of Ontario the official language is English, but there are an estimated North America, Franco-Ontariansthe Province of Manitoba co-official as de jure with Englishthe French West Indies and Saint-Pierre et Miquelonas well as North America US state of Louisiana, where French is also an official language. Canada shows significant growth in the sectors of services, mining and manufacturing. Inexplicably, Vineland was abandoned after only a few years. Between and Frobisher as well as John Davis explored along the Atlantic coast. Central Intelligence Agence. -
Inherited Zircons Reveal a Gondwana Continental Fragment Beneath East Java, Indonesia ⁎ H.R
Earth and Planetary Science Letters 258 (2007) 269–282 www.elsevier.com/locate/epsl The deep crust beneath island arcs: Inherited zircons reveal a Gondwana continental fragment beneath East Java, Indonesia ⁎ H.R. Smyth a, , P.J. Hamilton b, R. Hall a, P.D. Kinny b a SE Asia Research Group, Royal Holloway University of London, Egham, Surrey TW200EX, UK b Department of Applied Geology, Curtin University of Technology, Perth 6845, Australia Received 21 November 2006; received in revised form 21 March 2007; accepted 21 March 2007 Available online 1 April 2007 Editor: R.W. Carlson Abstract Inherited zircons in Cenozoic sedimentary and igneous rocks of East Java range in age from Archean to Cenozoic. The distribution of zircons reveals two different basement types at depth. The igneous rocks of the Early Cenozoic arc, found along the southeast coast, contain only Archean to Cambrian zircons. In contrast, clastic rocks of north and west of East Java contain Cretaceous zircons, which are not found in the arc rocks to the south. The presence of Cretaceous zircons supports previous interpretations that much of East Java is underlain by arc and ophiolitic rocks, accreted to the Southeast Asian margin during Cretaceous subduction. However, such accreted material cannot account for the older zircons. The age populations of Archean to Cambrian zircons in the arc rocks are similar to Gondwana crust. We interpret the East Java Early Cenozoic arc to be underlain by a continental fragment of Gondwana origin and not Cretaceous material as previously suggested. Melts rising through the crust, feeding the Early Cenozoic arc, picked up the ancient zircons through assimilation or partial melting. -
Carbon and Strontium Isotope Stratigraphy of the Permian from Nevada and China: Implications from an Icehouse to Greenhouse Transition
Carbon and strontium isotope stratigraphy of the Permian from Nevada and China: Implications from an icehouse to greenhouse transition Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Kate E. Tierney, M.S. Graduate Program in the School of Earth Sciences The Ohio State University 2010 Dissertation Committee: Matthew R. Saltzman, Advisor William I. Ausich Loren Babcock Stig M. Bergström Ola Ahlqvist Copyright by Kate Elizabeth Tierney 2010 Abstract The Permian is one of the most important intervals of earth history to help us understand the way our climate system works. It is an analog to modern climate because during this interval climate transitioned from an icehouse state (when glaciers existed extending to middle latitudes), to a greenhouse state (when there were no glaciers). This climatic amelioration occurred under conditions very similar to those that exist in modern times, including atmospheric CO2 levels and the presence of plants thriving in the terrestrial system. This analog to the modern system allows us to investigate the mechanisms that cause global warming. Scientist have learned that the distribution of carbon between the oceans, atmosphere and lithosphere plays a large role in determining climate and changes in this distribution can be studied by chemical proxies preserved in the rock record. There are two main ways to change the distribution of carbon between these reservoirs. Organic carbon can be buried or silicate minerals in the terrestrial realm can be weathered. These two mechanisms account for the long term changes in carbon concentrations in the atmosphere, particularly important to climate.