| 共和──湟源地区近震波速及湟源地区地壳厚度的测定 |
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| 引用本文： | 都昌庭. 共和──湟源地区近震波速及湟源地区地壳厚度的测定[J]. 高原地震, 1996, 0(1) |
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| 作者姓名： | 都昌庭 |
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| 作者单位： | 青海省地震局 |
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| 摘 要： | 本文选取湟源台５７３型地震仪在１９９０—１９９１年间记录的４９个共和地震和记录到ＰＮ震相的２５个地震资料，通过计算，得到共和——湟源之间直达波的平均传播速度为；Ｖ（ｐｇ）＝６．７６ｋｍ／ｓ、Ｖ（ｓｇ）＝３．８４ｋｍ／ｓ，湟源地区的地壳厚度为６１ｋｍ。
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| 关 键 词： | 近震波速，地壳厚度 |
DETERMINATION THE NEAR SHOCK VELOCITY IN GONGHE-HUANGYUAN AREA AND THE CRUSTALTHICKNESS IN HUANGYUAN AREA |
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| Du Changting. DETERMINATION THE NEAR SHOCK VELOCITY IN GONGHE-HUANGYUAN AREA AND THE CRUSTALTHICKNESS IN HUANGYUAN AREA[J]. Plateau Earthquake Research, 1996, 0(1) |
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| Authors: | Du Changting |
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| Abstract: | The paper chooses 49 of earthquakes Gonghe seismic sequence recorded by 573 seismograph from 1990 to 1991 and 25 seismic data which were recorded PN seismic phase. By calculated,average velocity of direct wave between Gonghe and Huangyuan is;V(pg)= 6. 76km/s,V(sg)= 3.84km/s,the crustal thickness in Huangyuan area is 61km. |
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| Keywords: | Near shock velocity:Crustal thickness |
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