[[sponsorship]]地球科學研究所[[note]]已出版;[SCI];有審查制度;具代表性[[note]]http://gateway.isiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=Drexel&SrcApp=hagerty_opac&KeyRecord=0148-0227&DestApp=JCR&RQ=IF_CAT_BOXPLO
The characterization of magnetic minerals in rocks often uses methods that measure induced magnetiza...
http://deepblue.lib.umich.edu/bitstream/2027.42/8333/5/bad6081.0001.001.pdfhttp://deepblue.lib.umich...
The structure of the iron oxyhydroxide called feroxyhyte (δ-FeOOH), which shows an elusive X-ray po...
First-order reversal curve (FORC) diagrams have become a standard tool in rock magnetism, yet magnet...
First-order reversal curve (FORC) diagrams have become a standard tool in rock magnetism, yet magnet...
[1] First-order reversal curve (FORC) diagrams have become a standard tool in rock magnetism, yet ma...
First-order reversal curve (FORC) diagrams for mixtures of different magnetic phases and bimodal dis...
First-order reversal curve (FORC) diagrams for mixtures of different magnetic phases and bimodal dis...
[[sponsorship]]地球科學研究所[[note]]已出版;[SCI];有審查制度;不具代表性[[note]]http://gateway.isiknowledge.com/gateway/G...
Hematite carries magnetic signals of interest in tectonic, paleoclimatic, paleomagnetic, and planeta...
Common Forms/Occurrences: Mainly of sedimentary origin Useful Identification Test: May be attrac...
Common Forms/Occurrences: Mainly of sedimentary origin Useful Identification Test: May be attrac...
Common Forms/Occurrences: Mainly of sedimentary origin Useful Identification Test: May be attrac...
The iron oxides hematite, magnetite, and goethite were studied with density functional theory to est...
The most frequent crystallographic preferred orientations developed during the progressive phase tra...
The characterization of magnetic minerals in rocks often uses methods that measure induced magnetiza...
http://deepblue.lib.umich.edu/bitstream/2027.42/8333/5/bad6081.0001.001.pdfhttp://deepblue.lib.umich...
The structure of the iron oxyhydroxide called feroxyhyte (δ-FeOOH), which shows an elusive X-ray po...
First-order reversal curve (FORC) diagrams have become a standard tool in rock magnetism, yet magnet...
First-order reversal curve (FORC) diagrams have become a standard tool in rock magnetism, yet magnet...
[1] First-order reversal curve (FORC) diagrams have become a standard tool in rock magnetism, yet ma...
First-order reversal curve (FORC) diagrams for mixtures of different magnetic phases and bimodal dis...
First-order reversal curve (FORC) diagrams for mixtures of different magnetic phases and bimodal dis...
[[sponsorship]]地球科學研究所[[note]]已出版;[SCI];有審查制度;不具代表性[[note]]http://gateway.isiknowledge.com/gateway/G...
Hematite carries magnetic signals of interest in tectonic, paleoclimatic, paleomagnetic, and planeta...
Common Forms/Occurrences: Mainly of sedimentary origin Useful Identification Test: May be attrac...
Common Forms/Occurrences: Mainly of sedimentary origin Useful Identification Test: May be attrac...
Common Forms/Occurrences: Mainly of sedimentary origin Useful Identification Test: May be attrac...
The iron oxides hematite, magnetite, and goethite were studied with density functional theory to est...
The most frequent crystallographic preferred orientations developed during the progressive phase tra...
The characterization of magnetic minerals in rocks often uses methods that measure induced magnetiza...
http://deepblue.lib.umich.edu/bitstream/2027.42/8333/5/bad6081.0001.001.pdfhttp://deepblue.lib.umich...
The structure of the iron oxyhydroxide called feroxyhyte (δ-FeOOH), which shows an elusive X-ray po...
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