FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2860877536> ?p ?o ?g. }

• W2860877536 endingPage "336" @default.
• W2860877536 startingPage "277" @default.
• W2860877536 abstract "This chapter reviews current knowledge of the permanent and induced magnetizations of terrestrial and extraterrestrial rocks and minerals. The emphasis is on recent developments and on aspects of rock magnetism that are most useful in magnetic anomaly interpretation and paleomagnetism. Beginning with atomic scale magnetism (diamagnetism, paramagnetism, ferromagnetism, antiferromagnetism, ferrimagnetism) and magnetic anisotropies (magnetocrystalline, magnetoelastic), we show how nanometer-scale magnetic domains develop in response to self-demagnetization. The very different responses of magnetic crystals subdivided into domains (multidomain or MD grains) and smaller crystals that resist such subdivision (single-domain or SD grains) to magnetic fields, temperature, and time are all important in paleomagnetism. SD grains are capable of preserving a record of the ancient magnetic field of the Earth and other planets that is stable throughout geological time while MD grains preserve a much inferior record or no record at all. The grain size that separates SD from MD behavior varies from mineral to mineral, being smallest in strongly magnetic minerals like iron and magnetite and largest in weakly magnetic minerals like hematite. Magnetic stability, both short term and long term, is much affected by temperature and many important phenomena, for example, blocking of stable remanent magnetization and the Hopkinson peak in induced magnetization, occur just below the Curie temperature, which also varies from one mineral to another. We show that fundamental principles underlie standard paleomagnetic ‘cleaning’ techniques and laboratory stability tests, as well as the best methods of determining paleomagnetic field direction and intensity. Next we review the latest developments in knowledge about the basic processes by which igneous, sedimentary and metamorphic rocks are magnetized and partially remagnetized in nature. These include thermoremanent, viscous, thermoviscous, chemical and depositional/postdepositional magnetizations. Finally we summarize our current knowledge and major unsolved problems for the future." @default.
• W2860877536 created "2018-07-19" @default.
• W2860877536 creator A5027016066 @default.
• W2860877536 creator A5085257858 @default.
• W2860877536 date "2007-01-01" @default.
• W2860877536 modified "2023-09-30" @default.
• W2860877536 title "Magnetizations in Rocks and Minerals" @default.
• W2860877536 cites W1514044661 @default.
• W2860877536 cites W1518946904 @default.
• W2860877536 cites W1591480399 @default.
• W2860877536 cites W1964114137 @default.
• W2860877536 cites W1965754818 @default.
• W2860877536 cites W1966765391 @default.
• W2860877536 cites W1969034680 @default.
• W2860877536 cites W1969470869 @default.
• W2860877536 cites W1970888972 @default.
• W2860877536 cites W1971725459 @default.
• W2860877536 cites W1973578650 @default.
• W2860877536 cites W1974627420 @default.
• W2860877536 cites W1975908710 @default.
• W2860877536 cites W1976087111 @default.
• W2860877536 cites W1976241867 @default.
• W2860877536 cites W1983355514 @default.
• W2860877536 cites W1983989686 @default.
• W2860877536 cites W1984471561 @default.
• W2860877536 cites W1984765308 @default.
• W2860877536 cites W1988183821 @default.
• W2860877536 cites W1989314379 @default.
• W2860877536 cites W1989920955 @default.
• W2860877536 cites W1991880341 @default.
• W2860877536 cites W1992545002 @default.
• W2860877536 cites W1992733055 @default.
• W2860877536 cites W1994153906 @default.
• W2860877536 cites W1994824425 @default.
• W2860877536 cites W1995941045 @default.
• W2860877536 cites W1997581680 @default.
• W2860877536 cites W1997832792 @default.
• W2860877536 cites W1998298788 @default.
• W2860877536 cites W1998635456 @default.
• W2860877536 cites W2001203090 @default.
• W2860877536 cites W2001860915 @default.
• W2860877536 cites W2001935526 @default.
• W2860877536 cites W2003069188 @default.
• W2860877536 cites W2003255082 @default.
• W2860877536 cites W2003600396 @default.
• W2860877536 cites W2007180232 @default.
• W2860877536 cites W2007729929 @default.
• W2860877536 cites W2011138323 @default.
• W2860877536 cites W2011152079 @default.
• W2860877536 cites W2011641927 @default.
• W2860877536 cites W2011688765 @default.
• W2860877536 cites W2013086350 @default.
• W2860877536 cites W2013553127 @default.
• W2860877536 cites W2015389513 @default.
• W2860877536 cites W2015895598 @default.
• W2860877536 cites W2018205219 @default.
• W2860877536 cites W2018264648 @default.
• W2860877536 cites W2018379441 @default.
• W2860877536 cites W2022068308 @default.
• W2860877536 cites W2023588009 @default.
• W2860877536 cites W2023669973 @default.
• W2860877536 cites W2029067829 @default.
• W2860877536 cites W2030166124 @default.
• W2860877536 cites W2033239846 @default.
• W2860877536 cites W2033759719 @default.
• W2860877536 cites W2035791138 @default.
• W2860877536 cites W2037468177 @default.
• W2860877536 cites W2037918657 @default.
• W2860877536 cites W2038200418 @default.
• W2860877536 cites W2039304582 @default.
• W2860877536 cites W2039681241 @default.
• W2860877536 cites W2041883260 @default.
• W2860877536 cites W2042225110 @default.
• W2860877536 cites W2042522231 @default.
• W2860877536 cites W2042730563 @default.
• W2860877536 cites W2043581256 @default.
• W2860877536 cites W2045044499 @default.
• W2860877536 cites W2046935351 @default.
• W2860877536 cites W2049385523 @default.
• W2860877536 cites W2051033070 @default.
• W2860877536 cites W2052128667 @default.
• W2860877536 cites W2052518277 @default.
• W2860877536 cites W2053452930 @default.
• W2860877536 cites W2054341587 @default.
• W2860877536 cites W2055329250 @default.
• W2860877536 cites W2055781465 @default.
• W2860877536 cites W2055926314 @default.
• W2860877536 cites W2056088414 @default.
• W2860877536 cites W2056098342 @default.
• W2860877536 cites W2056525512 @default.
• W2860877536 cites W2057482142 @default.
• W2860877536 cites W2058151373 @default.
• W2860877536 cites W2058258404 @default.
• W2860877536 cites W2062761864 @default.
• W2860877536 cites W2063456902 @default.
• W2860877536 cites W2064862074 @default.
• W2860877536 cites W2067437284 @default.
• W2860877536 cites W2068051936 @default.

• next