释义 |
Definition of magnetite in English: magnetitenoun ˈmaɡnɪtʌɪtˈmæɡnəˌtaɪt mass nounA grey-black magnetic mineral which consists of an oxide of iron and is an important form of iron ore. 磁铁矿 Example sentencesExamples - In the left test tube, a magnet attracts magnetite, the byproduct of Strain 121's respiration of iron oxide and offers a tell-tale sign of life in the tube.
- The dominant carrier of remanent magnetization of the doleritic rocks is relatively pure magnetite of pseudo-single domain size, and the characteristic remanent magnetizations are typically well defined and unidirectional.
- The new ‘evidence’ is tiny (one-millionth of an inch in diameter) crystals of magnetite, a magnetic oxide of iron.
- More important, because the presence of magnetite gives the basalt measurable magnetic properties, these newly discovered magnetic variations provided another means to study the deep ocean floor.
- This colour change occurs over only a few metres on the ground and is probably related to the reduction of hematite to magnetite.
- The sample is composed of K-feldspar, plagioclase and quartz with accessory apatite, magnetite, titanite, zircon and secondary epidote.
- Spinels in the country rock are essentially pure magnetite.
- The majority of the rhyolites are porphyritic and contain phenocrysts of one or more of the following: plagioclase, clinopyroxene, magnetite, quartz and sanidine, plus accessory apatite and zircon.
- In part, the hypothesis involved tiny grains of the naturally magnetic mineral magnetite, which is commonly found in basalt (a high-temperature volcanic rock that makes up oceanic crust).
- Along the contact zone the limestones were recrystallized into a cloudy white, massive calcite containing grossular, epidote, magnetite, quartz, and tremolite.
- The replacement of the authigenic magnetite by hematite probably occurred at the same time as the specular hematite that surrounds the dolomite grains.
- The third potential way the hematite could have formed is by oxidation of a mineral called magnetite in basalt and lavas.
- Nearby is a magnet, composed of natural magnetite, that once belonged to Lomonosov.
- The magnetite, uralite, and other minerals can be exposed by etching away the enclosing calcite with hydrochloric acid.
- Lodestones are simply naturally occurring magnets composed of the magnetic mineral magnetite.
- Microscopic analyses reveal that the oxide mineralogy of the dolerites is dominated by magnetite and ilmenite.
- The sedimentary clasts also contain abundant opaque minerals, chiefly magnetite.
- The claims centre on a mineral with a high iron content called magnetite, which is found embedded in the Martian rock in an unusual form.
- The palaeomagnetic analyses of this study have revealed that the dominant carrier of remanent magnetization of the Whin Sill dolerite is relatively pure magnetite in the pseudo-single domain size range.
- Chemically, Strain 121's respiration process reduces ferric iron to ferrous iron and forms the mineral magnetite, the source of most of the magnetic material deposited on Earth some two billion years ago.
OriginMid 19th century: from magnet + -ite1. Definition of magnetite in US English: magnetitenounˈmæɡnəˌtaɪtˈmaɡnəˌtīt A gray-black magnetic mineral which consists of an oxide of iron and is an important form of iron ore. 磁铁矿 Example sentencesExamples - Spinels in the country rock are essentially pure magnetite.
- In part, the hypothesis involved tiny grains of the naturally magnetic mineral magnetite, which is commonly found in basalt (a high-temperature volcanic rock that makes up oceanic crust).
- The replacement of the authigenic magnetite by hematite probably occurred at the same time as the specular hematite that surrounds the dolomite grains.
- Lodestones are simply naturally occurring magnets composed of the magnetic mineral magnetite.
- The palaeomagnetic analyses of this study have revealed that the dominant carrier of remanent magnetization of the Whin Sill dolerite is relatively pure magnetite in the pseudo-single domain size range.
- The majority of the rhyolites are porphyritic and contain phenocrysts of one or more of the following: plagioclase, clinopyroxene, magnetite, quartz and sanidine, plus accessory apatite and zircon.
- The new ‘evidence’ is tiny (one-millionth of an inch in diameter) crystals of magnetite, a magnetic oxide of iron.
- Nearby is a magnet, composed of natural magnetite, that once belonged to Lomonosov.
- The sample is composed of K-feldspar, plagioclase and quartz with accessory apatite, magnetite, titanite, zircon and secondary epidote.
- Microscopic analyses reveal that the oxide mineralogy of the dolerites is dominated by magnetite and ilmenite.
- The claims centre on a mineral with a high iron content called magnetite, which is found embedded in the Martian rock in an unusual form.
- This colour change occurs over only a few metres on the ground and is probably related to the reduction of hematite to magnetite.
- More important, because the presence of magnetite gives the basalt measurable magnetic properties, these newly discovered magnetic variations provided another means to study the deep ocean floor.
- The sedimentary clasts also contain abundant opaque minerals, chiefly magnetite.
- The third potential way the hematite could have formed is by oxidation of a mineral called magnetite in basalt and lavas.
- The magnetite, uralite, and other minerals can be exposed by etching away the enclosing calcite with hydrochloric acid.
- In the left test tube, a magnet attracts magnetite, the byproduct of Strain 121's respiration of iron oxide and offers a tell-tale sign of life in the tube.
- Along the contact zone the limestones were recrystallized into a cloudy white, massive calcite containing grossular, epidote, magnetite, quartz, and tremolite.
- Chemically, Strain 121's respiration process reduces ferric iron to ferrous iron and forms the mineral magnetite, the source of most of the magnetic material deposited on Earth some two billion years ago.
- The dominant carrier of remanent magnetization of the doleritic rocks is relatively pure magnetite of pseudo-single domain size, and the characteristic remanent magnetizations are typically well defined and unidirectional.
OriginMid 19th century: from magnet + -ite. |