Sentence examples for magnetic experiments and from inspiring English sources

We also conducted a suite of rock magnetic experiments and an observation with scanning electron microscope, to characterize rock magnetic properties of the samples.

From each sample, a small slice was cut for a thin section and rock magnetic experiments, and the remainder was used in paleointensity experiments.

This is followed by a description of the magnetic experiments and analysis, as well as a discussion of the size dependent magnetic properties.

A suite of the rock magnetic experiments and the SEM observations elucidate that dominant magnetic carriers of the floor surface samples are Ti-poor titanomagnetite grains in approximately 10 nm size, with SD and/or SP states.

A suite of the rock magnetic experiments and the scanning electron microscope observations elucidate that dominant magnetic carriers of the floor surface samples are Ti-poor titanomagnetite grains in approximately 10 nm size with single-domain and/or super-paramagnetic states, whereas contributions of multi-domain grains seem to be relatively large for the −20-cm level samples.

Based on rock-magnetic experiments and microscopic observations, it is revealed that the measured paleointensity is carried by single-domain (titano magnetite.

Additionally, we performed rock magnetic experiments, mineral analysis, and paleodirection measurement to evaluate the suitability of the baked clay samples for paleointensity experiments and hence confirmed that the sample properties were ideal for performing paleointensity experiments.

We also performed a variety of rock magnetic experiments, mineral analysis, and paleodirection measurements to evaluate the suitability of baked clay samples for paleointensity experiments.

From rock magnetic experiments, mineral analysis, and paleodirection measurements, it was revealed that the main magnetic mineral in the samples is titanomagnetite, the alteration during heating is very small, and the recorded NRM is the only single component of TRM acquired in the operating time at temperatures greater than 1000 °C.

Rock magnetic experiments, electron probe microanalysis, and scanning electron microscopy revealed characteristic signatures of (post- pedogenic influences on the original sedimentary fabric.

Figure 3 Photographs showing the samples used for archeointensity (paleointensity) and rock magnetic experiments.