Sentence examples for oceanic boundary from inspiring English sources

The two convergences are well defined and important oceanic boundary zones that profoundly affect climates, marine life, bottom sedimentation, and ice-pack and iceberg drift.

However, the Lg propagation to the Japanese main island of Honshu was totally blocked because it crosses the continental to oceanic boundary surrounding the Sea of Japan.

We believe that the problems arise from subtle issues in the structural model, such as the delicate curvature of the Moho along the continental to oceanic boundary.

We also find that along the continent to oceanic boundary on the Pacific Ocean side of Japan (which corresponds roughly to the 1,000-m 1,000-mh contour of the water depth), the Lg wave propagatisodepthotally blocontour

This indicates that the risk for severe weather is also valid in that general area of the other side of the border or oceanic boundary.

By far the most abundant organic acids are the C1 and C2 monocarboxylic acids, formic acid (HCOOH) and acetic acid (CH3COOH), which show mixing ratios in the gas phase ranging up to 20 ppb over land 1, 2 and down to 0.2 ppb in the remote oceanic boundary layer or troposphere.

Since the mid-1970s, researchave have studied realistic models of the Earth's structure that include continental and oceanic boundaries, mountains, and river valleys rather than simple structures such as those involving variation only with depth.

The integration time was relatively short, so open oceanic boundaries were used in a series of numerical simulations.

However, the Lg wave propagation to the Japanese main island of Honshu is totally blocked as it crosses the continental-oceanic boundary surrounding the Sea of Japan.

We set a constant trace element composition on the oceanic side boundary (as with water), which consists of oceanic crust composed of altered oceanic crust (Kelley et al. 2003) and a depleted MORB mantle (DMM) (Workman and Hart 2005).

In order to simulate subduction of the Pacific Plate beneath northeast (NE) Japan, a geotherm for the plate age of 130 million years (Myr) is applied to the oceanic side boundary, based on the one-dimensional cooling model of semi-infinite half-space (Turcotte and Shubert 1982) with an initial potential temperature of 1,350°C (Parsons and Sclater 1977).