mantle zone

基本解釋

A sharp temperature increase across the mid-mantle transition zone inhibits a simple downward-extrapolation from the near surface data.
中地幔過渡帶有一個溫度突然增加，因此不能根據(jù)近地表數(shù)據(jù)向下做簡單的外推。
The calculated results of temperature and pressure from mineralogical chemistry show that magmatic source should lie in crust-mantle intermediate zone.
從礦物化學所獲得的溫度-壓力計算結(jié)果表明：巖漿來源應(yīng)位于殼幔過渡帶。
According to dissecting depth of the zone of faults, the two zones of faults with upwelling of magma were transcrust (crust-upper mantle zone of faults).
根據(jù)斷裂帶切割深度，認定這兩個斷裂帶均為超殼斷裂，且都有巖漿上涌。
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