Rock Magnetism and Palaeomagnetism of Meteorite Impact Craters in India
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Geochemical Characterization of Moldavites from a New Locality, the Cheb Basin, Czech Republic
Geochemical characterization of moldavites from a new locality, the Cheb Basin, Czech Republic Item Type Article; text Authors Řanda, Zdeněk; Mizera, Jiři; Frána, Jaroslav; Kučera, Jan Citation Řanda, Z., Mizera, J., Frána, J. and Kučera, J. (2008), Geochemical characterization of moldavites from a new locality, the Cheb Basin, Czech Republic. Meteoritics & Planetary Science, 43(3), 461-477. DOI 10.1111/j.1945-5100.2008.tb00666.x Publisher The Meteoritical Society Journal Meteoritics & Planetary Science Rights Copyright © The Meteoritical Society Download date 30/09/2021 11:07:40 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/656405 Meteoritics & Planetary Science 43, Nr 3, 461–477 (2008) AUTHOR’S PROOF Abstract available online at http://meteoritics.org Geochemical characterization of moldavites from a new locality, the Cheb Basin, Czech Republic ZdenÏk ÿANDA1, Ji¯í MIZERA1, 2*, Jaroslav FRÁNA1, and Jan KU»ERA1 1Nuclear Physics Institute, Academy of Sciences of the Czech Republic, 250 68 ÿež, Czech Republic 2Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, V HolešoviËkách 41, 182 09 Praha 8, Czech Republic *Corresponding author. E-mail: [email protected] (Received 02 June 2006; revision accepted 15 July 2007) Abstract–Twenty-three moldavites from a new locality, the Cheb Basin in Western Bohemia, were analyzed by instrumental neutron activation analysis for 45 major and trace elements. Detailed comparison of the Cheb Basin moldavites with moldavites from other substrewn fields in both major and trace element composition shows that the Cheb Basin is a separate substrewn field. -
The Tennessee Meteorite Impact Sites and Changing Perspectives on Impact Cratering
UNIVERSITY OF SOUTHERN QUEENSLAND THE TENNESSEE METEORITE IMPACT SITES AND CHANGING PERSPECTIVES ON IMPACT CRATERING A dissertation submitted by Janaruth Harling Ford B.A. Cum Laude (Vanderbilt University), M. Astron. (University of Western Sydney) For the award of Doctor of Philosophy 2015 ABSTRACT Terrestrial impact structures offer astronomers and geologists opportunities to study the impact cratering process. Tennessee has four structures of interest. Information gained over the last century and a half concerning these sites is scattered throughout astronomical, geological and other specialized scientific journals, books, and literature, some of which are elusive. Gathering and compiling this widely- spread information into one historical document benefits the scientific community in general. The Wells Creek Structure is a proven impact site, and has been referred to as the ‘syntype’ cryptoexplosion structure for the United State. It was the first impact structure in the United States in which shatter cones were identified and was probably the subject of the first detailed geological report on a cryptoexplosive structure in the United States. The Wells Creek Structure displays bilateral symmetry, and three smaller ‘craters’ lie to the north of the main Wells Creek structure along its axis of symmetry. The question remains as to whether or not these structures have a common origin with the Wells Creek structure. The Flynn Creek Structure, another proven impact site, was first mentioned as a site of disturbance in Safford’s 1869 report on the geology of Tennessee. It has been noted as the terrestrial feature that bears the closest resemblance to a typical lunar crater, even though it is the probable result of a shallow marine impact. -
Lechatelierite in Moldavite Tektites: New Analyses of Composition
52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 1580.pdf LECHATELIERITE IN MOLDAVITE TEKTITES: NEW ANALYSES OF COMPOSITION. Martin Molnár1, Stanislav Šlang2, Karel Ventura3. Kord Ernstson4.1Resselovo nám. 76, Chrudim 537 01, Czech Republic ([email protected]) 2Center of Materials and Nanotechnologies, University of Pardubice, 532 10 Pardubice, Czech Republic, [email protected] 3Faculty of Chemical Technology, University of Pardubice, 530 02 Pardubice, Czech Republic, [email protected]. 4University of Würzburg, D-97074 Würzburg, Deutschland ([email protected]) Introduction: Moldavites are tektites with a Experiments and Results: Experiments 1 and 2 - beautiful, mostly green discoloration and a very the boron question. The question of lowering the pronounced sculpture (Fig.1), which have been studied melting point and acid resistance led to the possibility many times e.g. [1-3]). of adding boron. The experiment 1 on a moldavite plate etched in 15%-HF to expose the lechatelierite was performed by laser ablation spectrometry and showed B2O3 concentration of >1%. In experiment 2, 38 g of lechatelierite fragments were then separated from 482 g of pure moldavite, and after the boron Fig. 1. Moldavites from Besednice analyzed in this content remained high (Tab. 2), the remaining carbon study. Scale bar 1 cm. was washed away. The analysis in Tab. 3 shows According to the most probable theory, they were remaining low boron content, which is obviously formed 14.5 million years ago together with the Ries bound to the carbon of the moldavites [8]. crater meteorite impact in Germany. They belong to the mid-European tektite strewn field and fell mostly in Bohemia. -
ABSTRACT 1 Terrestrial Impact Craters
MAPPING TERRESTRIAL IMPACT CRATERS WITH THE TANDEM-X DIGITAL ELEVATION MODEL Manfred Gottwald1, Thomas Fritz1, Helko Breit1, Birgit Schättler1, Alan Harris2 1German Aerospace Center, Remote Sensing Technology Institute, Oberpfaffenhofen, D-82234 Wessling, Germany 2German Aerospace Center, Institute of Planetary Research, Rutherfordstr. 2, D-12489 Berlin, Germany ABSTRACT We use the global digital elevation model (DEM) generated in the TanDEM-X mission for map- ping the confirmed terrestrial impact structures in the Earth Impact Database of the Planetary and Space Science Center (PASSC) at the University of New Brunswick, Canada. The TanDEM- X mission generates a global DEM with unprecedented properties. The achieved global coverage together with the improved accuracy (in the sub-10 m range) and spatial resolution (12 m at the equator) opens new opportunities in impact crater research based on terrestrial space-borne remote sensing data. It permits both for simple and complex craters investigations of the mor- phology of the particular structure (rim height, central uplift, ring-like patterns, elevation pro- files) and of the surrounding terrain (local deformation, drainage patterns) of outstanding quali- ty. 1 Terrestrial Impact Craters Earth, in contrast, the crust underwent continuous modification due to various processes such as plate 1.1 Impact Crater Record tectonics, erosion, sedimentation and glaciation. This prevented the development of an unbiased impact Terrestrial impact craters are the relics of collisions of record. Only the ancient continental shields provide the Earth with Solar System objects of different sizes. opportunities for detecting very old impact structures. Such collisions were frequent in the distant past when In other areas, craters of a certain size have remained the Solar System was young but even today solid bod- sufficiently intact only if they were formed rather re- ies from interplanetary space occasionally hit the ter- cently or if their large size has prevented them from restrial surface. -
The Geophysical Signature of Impact Craters
The geophysical signature of impact craters Stephanie Werner Observation, geophysical techniques and implications • Gravity Anomalies • Magnetic Anomalies • Seismic profiling • Electrical /Electromagnetic • Magnetotelluric • Ground Penetrating Radar •Radiometric •… Crater Formation Process Observations:Observations: PhysicalPhysical Shape: circular features Moltke Tycho (2.7 mi) (53 mi) Inverted Stratigraphy: Meteor Crater first recognized by Barringer (only for well preserved craters) Material displacement: Solid material broken up and ejected outside the crater: breccia, tektites Slide from B. Pierazzo Observations:Observations: ShockShock EvidenceEvidence Shatter cones: conical fractures with typical markings produced by shock waves Shocked Material: shocked quartz high pressure minerals Melt Rocks: may result from shock and friction Slide from B. Pierazzo Observations:Observations: GeophysicalGeophysical datadata Gravity anomaly: based on density variations of materials Magnetic: based on general variation of magnetic properties of materials Seismic: sound waves reflection and refraction from subsurface layers with different characteristics Slide from B. Pierazzo Gravity Anomalies Gravity • craters are relatively shallow features, but depressions • associated to brecciation and fracturing, extending to significant depth below the crater floor • fractured rock is less dense than unaltered rock material • dependent size and morphology, density contrast and burial depth – circular negative gravity anomaly Gravity anomaly: Simple crater -
Twinning, Reidite, and Zro in Shocked Zircon from Meteor Crater
Transformations to granular zircon revealed: Twinning, reidite, and ZrO2 in shocked zircon from Meteor Crater (Arizona, USA) Aaron J. Cavosie1,2,3, Nicholas E. Timms1, Timmons M. Erickson1, Justin J. Hagerty4, and Friedrich Hörz5 1TIGeR (The Institute for Geoscience Research), Department of Applied Geology, Curtin University, Perth, WA 6102, Australia 2NASA Astrobiology Institute, Department of Geoscience, University of Wisconsin–Madison, Madison, Wisconsin 53706, USA 3Department of Geology, University of Puerto Rico–Mayagüez, Mayagüez, Puerto Rico 00681, USA 4U.S. Geological Survey (USGS) Astrogeology Science Center, Flagstaff, Arizona 86001, USA 5NASA Johnson Space Center, Science Department/Jets/HX5/ARES, Houston, Texas 77058, USA ABSTRACT Granular zircon in impact environments has long been recognized but remains poorly A N35° 2.0’ W111° 0.9’ understood due to lack of experimental data to identify mechanisms involved in its genesis. Meteor Crater in Arizona (USA) contains abundant evidence of shock metamorphism, includ- N ing shocked quartz, the high-pressure polymorphs coesite and stishovite, diaplectic SiO2 glass, and lechatelierite (fused SiO2). Here we report the presence of granular zircon, a new shocked-mineral discovery at Meteor Crater, that preserve critical orientation evidence of specific transformations that occurred during formation at extreme impact conditions. The zircon grains occur as aggregates of sub-micrometer neoblasts in highly shocked Coconino Sandstone (CS) comprised of lechatelierite. Electron backscatter diffraction shows that each MCC2 site grain consists of multiple domains, some with boundaries disoriented by 65° around <110>, (main shaft) a known {112} shock-twin orientation. Other domains have {001} in alignment with {110} of neighboring domains, consistent with the former presence of the high-pressure ZrSiO4 polymorph reidite. -
Comment Article Evidence That Lake Cheko Is Not an Impact Crater
doi: 10.1111/j.1365-3121.2008.00791.x Comment article Evidence that Lake Cheko is not an impact crater G. S. Collins,1 N. Artemieva,2 K. Wu¨ nnemann,3 P. A. Bland,1 W. U. Reimold,3 and C. Koeberl4 1Impacts and Astromaterials Research Centre, Department of Earth Science and Engineering, Imperial College London, SW7 2AZ London, UK; 2Institute for the Dynamics of Geospheres, Russian Academy of Sciences, Moscow, Russia; 3Museum for Natural History, Humboldt University, Invalidenstrasse 43, 10115 Berlin, Germany; 4Center of Earth Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria ABSTRACT In a provocative paper Gasperini et al. (2007) suggest that Lake is required for an asteroid fragment to traverse the EarthÕs Cheko, a 300-m-wide lake situated a few kilometres down- atmosphere and reach the surface intact and with sufficient range from the assumed epicentre of the 1908 Tunguska event, velocity to excavate a crater the size of Lake Cheko. Inferred is an impact crater. In this response, we present several lines of tensile strengths of large stony meteorites during atmospheric observational evidence that contradicts the impact hypothesis disruption are 10–100 times lower. We therefore conclude that for the lakeÕs origin: un-crater-like aspects of the lake mor- Lake Cheko is highly unlikely to be an impact crater. phology, the lack of impactor material in and around the lake, and the presence of apparently unaffected mature trees close Terra Nova, 20, 165–168, 2008 to the lake. We also show that a tensile strength of 10–40 MPa over 170 confirmed impact structures The first piece of evidence does give Introduction on the Earth (Earth Impact Database, pause for thought, but could easily be An impact origin for Lake Cheko and 2007). -
Dating Ilumetsa Craters (Estonia) Based on Charcoal Emplaced Within Their Proximal Ejecta Blankets
Lunar and Planetary Science XLVIII (2017) 1879.pdf Dating Ilumetsa Craters (Estonia) DATING ILUMETSA CRATERS (ESTONIA) BASED ON CHARCOAL EMPLACED WITHIN THEIR PROXIMAL EJECTA BLANKETS. A. Losiak1, A. Jõeleht2, J. Plado2, M. Szyszka3, E.M. Wild4, M. Bronikowska3, C. Belcher5, K. Kirsimäe2, P. Steier4. 1Planetary Geology Lab, Institute of Geological Sciences, Polish Academy of Sciences, Poland ([email protected]); 2Department of Geology, University of Tartu, Estonia ([email protected], [email protected], [email protected]), 3Institute of Geology, Adam Mickiewicz University in Poznan ([email protected], [email protected]); 4VERA Laboratory, Faculty of Physics—Isotope Research & Nuclear Physics, University of Vienna ([email protected], [email protected]); 5wildFIRE Lab, Hatherly Laboratories, University of Exeter, UK ([email protected]). Introduction: The Ilumetsa crater field in SE Estonia The aim of this current study was to determine/confirm the consists of two structures with diameters of 75-80 m age of those structures by 14C dating of organic material (Põrguhaud /Hell's Grave /Ilumetsa Large (IL)) and ~50 m covered by the proximal ejecta and search for possible impact (Sügavhaud /The Deep Grave /Ilumetsa Small – (IS)) with true related charcoals. This approach was recently successfully depths of about 8 and 3.5 m, respectively [1, Fig. 1]. Both applied to dating crater Kaali Main [5]. Additionally, our study structures are surrounded with a rim up to a few meters high attempts to determine if Ilumetsa was indeed created during an which is highest in the eastern parts (max. -
A New Chronology for the Moon and Mercury
A new chronology for the Moon and Mercury Simone Marchi German Aerospace Center (DLR), Institute of Planetary Research, Rutherfordstr. 2, D-12489 Berlin Dipartimento di Astronomia, Universit`adi Padova, Vicolo dell’Osservatorio 2, I-35122 Padova [email protected] Stefano Mottola German Aerospace Center (DLR), Institute of Planetary Research, Rutherfordstr. 2, D-12489 Berlin Gabriele Cremonese INAF, Osservatorio Astronomico di Padova, Vicolo dell’Osservatorio 3, I-35122 Padova Matteo Massironi Dipartimento di Geoscienze, Universit`adi Padova, via Giotto 1, I-35137, Padova and Elena Martellato INAF, Osservatorio Astronomico di Padova, Vicolo dell’Osservatorio 3, I-35122 Padova ABSTRACT In this paper we present a new method for dating the surface of the Moon, obtained by modeling the incoming flux of impactors and converting it into a size distribution of resulting craters. We compare the results from this model with the standard chronology for the Moon showing their similarities and discrepancies. In particular, we find indications of a non-constant impactor flux in the last 500 Myr and also discuss the implications of our findings for the Late Heavy Bombardment hypothesis. We also show the potential of our model for accurate dating of other inner Solar System bodies, by applying it to Mercury. arXiv:0903.5137v1 [astro-ph.EP] 30 Mar 2009 Subject headings: solar system: general — planets and satellites: Earth, Mercury, Moon 1. Introduction the evolution of the Solar System and in particu- lar of our own planet, the Earth. Recently, thanks Craters are among the most spectacular surface to a fleet of new space missions (Mars Express features of the solid bodies of the Solar System. -
Keurusselkä - Distribution of Shatter Cones
Lunar and Planetary Science XXXVIII (2007) 1762.pdf KEURUSSELKÄ - DISTRIBUTION OF SHATTER CONES. S. Hietala 1 and J. Moilanen 2, 1Kiveläntie 2 B 13, FI-42700 Keuruu, Finland, [email protected], 2Vuolijoentie 2086, FI-91760 Säräisniemi, Finland, [email protected]. Introduction: Keurusselkä impact structure was from the impact point increases. We have come to con- discovered by authors in 2003 [1], [2]. Well-formed clusion that most distant shatter cone like features we shatter cones in situ and boulders confirmed impact have found so far are still related to the impact struc- origin. A breccia with multiple sets of planar deforma- ture but this must be studied more carefully in future. tion features (PDFs) in quartz grains support this con- We have also measured directions of shatter cones. clusion. Structure is located in Central Finland (cen- This is not a simple task since only measurements that tered at 62°08´N, 24°37´E). seem to make any sense are made along the topside Exposed bedrocks of the region are Paleoprotero- striation of a shatter cone. What is the true topside of zoic granites and mica schists with volcanic inliers of the cone is not always so obvious. Central Finland Granitoid Complex. The age of the A breccia dike: In Autumn 2006 we discovered an granite basement is 1880 Ma. in situ breccia dike almost at the center of the structure. Precise age of the structure is unknown. It probably This is the first in situ breccia we have found and it is between 1880 - 600 Ma. 1880 Ma is the youngest may be impact related. -
The Geological Record of Meteorite Impacts
THE GEOLOGICAL RECORD OF METEORITE IMPACTS Gordon R. Osinski Canadian Space Agency, 6767 Route de l'Aeroport, St-Hubert, QC J3Y 8Y9 Canada, Email: [email protected] ABSTRACT 2. FORMATION OF METEORITE IMPACT STRUCTURES Meteorite impact structures are found on all planetary bodies in the Solar System with a solid The formation of hypervelocity impact craters has surface. On the Moon, Mercury, and much of Mars, been divided, somewhat arbitrarily, into three main impact craters are the dominant landform. On Earth, stages [3] (Fig. 2): (1) contact and compression, (2) 174 impact sites have been recognized, with several excavation, and (3) modification. A further stage of more new craters being discovered each year. The “hydrothermal and chemical alteration” is also terrestrial impact cratering record is critical for our considered as a separate, final stage in the cratering understanding of impacts as it currently provides the process (e.g., [4]), and is also described below. only ground-truth data on which to base interpretations of the cratering record of other planets and moons. In this contribution, I summarize the processes and products of impact cratering and provide and an up-to-date assessment of the geological record of meteorite impacts. 1. INTRODUCTION It is now widely recognized that impact cratering is a ubiquitous geological process that affects all planetary objects with a solid surface (e.g., [1]). One only has to look up on a clear night to see that impact structures are the dominant landform on the Moon. The same can be said of all the rocky and icy bodies in the solar system that have retained portions of their earliest crust. -
A Comparative Analysis of Two Early Palaeozoic Marine Impact Structures in Estonia, Baltic Sea: Neugrund and Kärdla
83 Bulletin of the Geological Society of Finland, Vol. 85, 2013, pp 83–101 A comparative analysis of two Early Palaeozoic marine impact structures in Estonia, Baltic Sea: Neugrund and Kärdla STEN SUUROJA1,2, KALLE SUUROJA1 AND TOM FLODÉN3 1 Geological Survey of Estonia, 12168 Tallinn, Estonia 2 Department of Geology, University of Tartu, Ravila 14a 50411, Estonia 3 Department of Geological Sciences, Stockholm University, 106 91 Stockholm, Sweden Abstract Kärdla and Neugrund are two Early Palaeozoic offshore impact structures located some 50 km apart along the Estonian coast of the Baltic Sea. They share many similarities but differing features are also found. The Kärdla impact structure is located at the NE coast of Hiiumaa Island (58°58’N, 22°46’E). The inner crater has a 4 km rim-to-rim diameter and a c. 130 m high central uplift, surrounded by a ring fault, c. 12 km in diameter. The well-preserved buried inner crater is outlined in the landscape by a circular ridge of uplifted bedrock. The perimeter of the outer crater is outlined on the seafloor by a semicircular ridge of narrow shoals. The variable height of the rim wall (50–240 m above the crystalline basement level) and the asymmetric location of the inner crater is obviously a result of an oblique impact in a layered target and partial collapse of the rim wall. Shortly after the impact in a shallow epicontinental sea during Late Ordovician time (c. 455 My), calcareous biodetritic muds were deposited and the crater was buried. The Neugrund impact structure is located in the seabed at the entrance of the Gulf of Finland (59°20’N, 23°31’E).