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Additional file 1. The ORF sequences of ETV4 and C-MYC, siRNAs sequences, and shRNA sequence for ETV4

Additional file 2. The primer sequences for qRT-PCR

This paper gives a report on the growth of saturable-absorber Cr, Ca:YAG by LPE. The analysis of the transmission spectra of epitaxially grown Cr, Ca:YAG shows that Cr4+ concentration ratio to total Cr concentration increase inversely as the concentration ratio of Ca and Cr decrease to Ca/Cr≈1. The transmission variation ΔT at 1.06 μm was measured to range between 5% and 30% according to the Cr concentration and the thickness of the epilayers. A discussion on the origin of a new absorption band at 760 nm is also presented, which suggests that Cr5+ ion could exist in the Cr, Ca:YAG in addition to Cr3+ and Cr4+.

The Fuzhou basin and its vicinities are located at the northern end of the southeastern coastal seismic zone of the mainland of China. By the joint explorations of high-resolution seismic refraction and wide-angle reflection/refraction as well as deep seismic reflection in the region, which is the first synthetic profile in China, its fine velocity structure and geometric structure from the ground to Moho discontinuity is obtained. The result shows that the crust is obviously layered with a thickness of about 32 km. Basically, it consists of two parts: upper crust and lower crust. The velocity of the upper crust is 5.9―6.2 km/s in which there is a 3―4-km-thick weak low-velocity layer between the depths of 10―15 km, while the velocity of the lower crust in the range of 6.3―7.2 km/s. There exists a strong velocity gradient layer about 3 km thick above the Moho discontinuity whose velocity increases from 6.5 to 7.27 km/s. There exist high-angle normal faults that are small in size and extend only in the shallow crust. These faults are the secondary developed on the hanging wall of westward dipping low-angle normal faults. Thus, their seismogenic ability is limited, however, there exists a high-angle deep fault in the crust from Changle-Zaoan fault zone to seashore fault zone. This deep fault has cut the interface between the upper and lower crusts and Moho discontinuity, and may be the deep structure to trigger destructive earthquake source in future to affect Fuzhou City. These results have advanced the detecting precision of the deep structure in the southeastern coastal seismic zone of the mainland of China. In the aspect of the combined feature of the deep and shallow extensional structures that consist of the westward dipping low-angle normal faults and secondary normal faults on their hanging walls in the upper crust, it is firstly obtained that a united structural interpretation has deepened the knowledge about the deep dynamic process in the southeastern coastal seismic zone. At the same time, in synthetic application of deep seismic detecting methods for deep tectonic background, it possesses a wide referenced meaning to the other regions.