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The intensity image of Me-ADOTA·Cl on SW on a silica protected gold mirror with SW orientation perpendicular to excitation light polarization is presented on the right.
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These two main directions were also measured in the quarries Heldenmühle and Neidenfels near Crailsheim showing a dominant NE-SW orientation.
Most eggs mapped in the field showed a long axis direction (axis a) of N44°, thus having a general NE-SW orientation which coincided with regional stress fields resulting from tectonic compression (Fig. 2B).
The long axis direction (axis a) of most eggs follows a general NE-SW orientation in the study area, which coincides with orientation of tectonic foliation in the region (Fig. 2B).
The NW-SE row orientation was stable at an average level and EW and NE-SW orientations were variable.
Also, recent work of Noten Van et al. (2013) has concluded that some normal faults were reactivated causing a left-lateral deformation in a transient strike-slip stress field with NE-SW orientations.
According to Schintgen and Förster (2013), the development of the Mesozoic TLB is attributed to a synsedimentary zone of weakness of SW-NE orientation along a Permian graben system.
Tempranillo, grafted onto 110R rootstocks and planted in 2007 on clay-loam soil with NE-SW row orientation, was used.
This study investigates the dominant orientations of morphological features and the relationship between these trends and the spatial orientation of tectonic structures in SW Jordan.
Two kinds of SWs were studied according to the relative orientation between the applied field and the waveguides: the transverse and the longitudinal cases.
Using a vector network analyzer, we measured SW transmission with the films magnetized in perpendicular orientation.
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