Abstract
Среднеглубинные землетрясения и связь сейсмичности зоны субдукции с метаморфизмом и глубинным флюидным режимом для Cеверного острова Новой Зеландии
Highlights
We applied descriptive statistics to the distributions of intermediate-depth earthquakes for a well-studied area of the North Island of New Zealand
Data on the density of the number of earthquakes are studied in the coordinates: depth - distance from the upper boundary of the submerged plate
This approach shows that some clusters of hypocenters are confined to the upper boundary of the subduction plate, while others are significantly distant from this boundary
Summary
We applied descriptive statistics to the distributions of intermediate-depth earthquakes for a well-studied area of the North Island of New Zealand. Data on the density of the number of earthquakes are studied in the coordinates: depth - distance from the upper boundary of the submerged plate.
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