edited by Sara S. Russell, Natural History Museum, London, Harold C. Connolly Jr., Rowan University, New Jersey, and Alexander N. Krot, University of Hawaii, Manoa.
وضعیت نشر و پخش و غیره
محل نشرو پخش و غیره
New York, NY :
نام ناشر، پخش کننده و غيره
Cambridge University Press,
تاریخ نشرو بخش و غیره
2018.
مشخصات ظاهری
نام خاص و کميت اثر
1 online resource
فروست
عنوان فروست
Cambridge planetary science ;
مشخصه جلد
22
یادداشتهای مربوط به کتابنامه ، واژه نامه و نمایه های داخل اثر
متن يادداشت
Includes bibliographical references and index.
یادداشتهای مربوط به مندرجات
متن يادداشت
Cover; Half-title; Series information; Title page; Copyright information; Table of contents; List of Contributors; 1 Introduction; Abstract; 1.1 Introduction; 1.2 A Brief History of Chondrule Research; 1.3 Primary Classification of Meteorites; 1.4 Secondary Classification; 1.5 Tertiary Classification; 1.6 Types of Chondrules; 1.6.1 Textural Types; 1.6.2 Chemical Types; 1.7 Refractory Inclusions; 1.8 Where Do Chondrites Come From?; References; Part I Observations of Chondrules
متن يادداشت
2 Multiple Mechanisms of Transient Heating Events in the Protoplanetary Disk: Evidence from Precursors of Chondrules and Igneous Ca, Al-Rich InclusionsAbstract; 2.1 Introduction; 2.2 Porphyritic Chondrules and Their Precursors; 2.2.1 Coarse-Grained Precursors of Porphyritic Chondrules; 2.2.1.1 Refractory Inclusions; 2.2.1.2 Precursors of Al-Rich Chondrules in Ordinary Chondrites; 2.2.1.3 Chondrules and Chondrule Fragments from Earlier Generations; 2.2.1.4 Fragments of Thermally Processed Planetesimals; 2.2.1.4.1 Clasts with Granoblastic Textures
متن يادداشت
2.2.1.4.2 Chromite-Rich Chondrules in Equilibrated Ordinary Chondrites: Formation by Melting of Metamorphosed Ordinary Chondrite-Like Materials2.2.2 Fine-Grained Precursors of Porphyritic Chondrules; 2.2.3 Was Matrix Material among Chondrule Precursors?; 2.2.4 Maintaining Chondrule Diversity; 2.3 Precursors of Igneous CAIs; 2.4 Precursors of Nonporphyritic Chondrules in CB and CH Carbonaceous Chondrites; 2.5 Recycling of CAIs in the CB Impact-Generated Gas-Melt Plume; 2.6 Discussion and Conclusions; Acknowledgments; References
متن يادداشت
3 Thermal Histories of Chondrules: Petrologic Observations and Experimental ConstraintsAbstract; 3.1 Introduction; 3.2 Observations and Experiments Relevant to Interpreting Thermal Histories; 3.2.1 Thermal Histories Determined from Textural Considerations; 3.2.1.1 Overview of Chondrule Petrology; 3.2.1.2 Dynamic Crystallization Experiments That Have Reproduced Chondrule Textures; 3.2.2 Thermal Histories Constrained from Mineral Chemistry and Zoning in Olivine and Pyroxene; 3.2.2.1 Growth Zoning; 3.2.2.2 Partition Coefficients; 3.2.2.3 Relict Grains
متن يادداشت
3.3 Constraints on Thermal Histories from Other Considerations3.3.1 Cu and Ga Diffusion Profiles of Metal Grains; 3.3.2 Exsolution Lamellae in Clinopyroxene; 3.3.3 Clinoenstatite Microstructure; 3.3.4 Presence of Glass and Critical Cooling Rate; 3.3.5 Dislocations in Olivine; 3.4 Discussion; 3.4.1 Continuous Linear Cooling Rates (Model A); 3.4.2 Nonlinear Cooling Rates, Constantly Decaying Cooling Rate (Model B); 3.4.3 Nonlinear Cooling Rates, Two-Stage Thermal History (Model C); 3.5 Summary and Outlook for Future Research; Acknowledgments; References
بدون عنوان
0
بدون عنوان
8
بدون عنوان
8
بدون عنوان
8
بدون عنوان
8
یادداشتهای مربوط به خلاصه یا چکیده
متن يادداشت
Chondrules are spherical silicate grains which formed from protoplanetary disk material, and as such provide an important record of the conditions of the Solar System in pre-planetary times. Chondrules are a major constituent in chondritic meteorites, however despite being recognised for over 200 years, their origins remain enigmatic. This comprehensive review describes state-of-the-art research into chondrules, bringing together leading cosmochemists and astrophysicists to review the properties of chondrules and their possible formation mechanisms based on careful observations of their chemistry, mineralogy, petrology and isotopic composition. Current and upcoming space missions returning material from chondritic asteroids and cometary bodies has invigorated research in this field, leading to new models and observations, and providing new insight into the conditions and timescales of the solar protoplanetary disk. Presenting the most recent advances, this book is an invaluable reference for researchers and graduate students interested in meteorites, asteroids, planetary accretion and solar system dynamics.