Adjective:

Eustatic,

eustatic শব্দের বাংলা অর্থ এর উদাহরণ:

Continental Shelves of the World: Their Evolution During the Last Glacio-Eustatic Cycle, Geological Society of London উদ্ধৃতি টেমপ্লেট ইংরেজি প্যারামিটার ।

eustatic's Usage Examples:

The term "eustatic" refers to global changes in sea level relative to a fixed point, such.

Production Research headed by Peter Vail published a monograph on global eustatic sea-level changes.

Rejuvenation may result from causes which are dynamic, eustatic or isostatic in nature.

The eustatic sea level is the distance from the center of the earth to the sea surface.

An increase of the eustatic sea level can be generated by decreasing.

Dalmatian types normally occur in high energy environments from where there is eustatic or isostatic change creating a submerging coastline.

activities can be extensively overcompensated by a eustatic sea level rise.

Thus, in areas of both eustatic and isostatic or tectonic influences, the course.

Global or eustatic sea level has fluctuated significantly over Earth's history.

eustatic) high-stand during the Holocene Epoch.

Modern understanding of the various factors involved in quantifying eustatic sea level, particularly.

level change that caused the submergence of a river valley may be either eustatic (where global sea levels rise), or isostatic (where the local land sinks).

In modern times, continents stand high, eustatic sea levels are low, and there are few inland seas, the largest being Hudson.

change in accommodation space (relative sea level, the combination of eustatic sea level and tectonic subsidence).

with eustatic sea level, which is a measure of the total mass or volume of the oceans.

Relative sea level can change by the processes changing eustatic sea.

meltwater at the end of ice ages is an example of eustatic sea level rise.

A second significant cause of eustatic sea level rise is thermal expansion of sea.

long temporal scales is mainly determined by tectonics or by changes in eustatic sea level.

The lake was formed by tectonic movements and eustatic sea level changes.

Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas.

It involved a global eustatic rise in sea level.

associated with meltwater pulse 1A are the highest known rates of post-glacial, eustatic sea level rise.