... zircon age spectra with peak ages near 1710 Ma. Igneous rocks that intrude the Vadito Group include the Cerro Alto metadacite, the Picuris Pueblo granite, and the Peñasco quartz monzonite and yield crystallization ages of 1710 ± 10 Ma, 1699 ± 3 Ma, and 1450 ± 10 Ma, respectively. Within the overlying...

... carbonaceous material, with two main broad bands at ∼1350 cm –1 and 1600 cm –1 consisting of a group of sub-peaks ( Fig. 1D ) that can be assigned to various modes of bond vibration in amorphous organic molecules ( Qu et al., 2015 , and references therein). Here we describe the spectra using the intensity...

... earthquake forecast maximum was 19% too low. TABLE 1 Least-squares Linear Fits to Fatality Rates (deaths/year) in Successive Centuries (± standard deviation) Time Interval <30K Old 30K Revised <5K Old <5K Revised 1500-1599 640±59 313±31 220±8 213±8 1600-1699...

... of bulk absorption comes at 1699 cm but these type of bands do not appear in case of vitrain and fusain. Bending vibration There are five absorption bands in the region 1647-1456 crn-! that are particu]arly diagnostic of aromatic structure. The pronounced peak found at about 1456 cm-] due...

... to any desired cavity size. 1.2 0.8 0.4 bJ C~ ~- 0 . 0 J [l_ E: 0.4 -0.8 tIIII[II 200 400 600 800 1000 1200 ] 400 1600 -1 .2 0 TIME SAMPLES 1.2 BACKGROUND 0.8 0.4 bJ E~ ~- 0 0 -0.4 -0.8 0 200 400 600 800 1000 ] 200 ] 400 1600 TIME SAMPLES RESONANCE Fro. 2. Seismograms for the mode n = 1 for water-filled...

...Fabrice Brunet; Vincent Bonneau; Tetsuo Irifune Abstract Syntheses along the Mg 3 Al 2 (SiO 4 ) 3 -Na 3 Al 2 (PO 4 ) 3 join were carried out in the 15–17 GPa range at temperatures between 1200 and 1600°C. An Na 3 Al 2 (PO 4 ) 3 compound of garnet-like structure, with a cubic-cell parameter...

.... (1978) . The upper mantle P velocity structure of the western United States , J. Geophys. Res. 83 , 1699 - 1712 . Golden P. Herrin E. (1989) . Development of an intelligent...

... MHz for the P-wave V P , and 0.5 MHz for the S-wave V s , and at hydrostatic stress σ h of 40 MPa. Figure 12. Depth plots of section from 1600 to 1700 m showing porosity, Biot’s coefficient, and modeled thermal conductivities from geometric mean...