Contents of this issue
Contents
- TITLE_SECTIONTitle Section
- CHAPTERSeismic Regions of the South Island of New Zealand
- ILLUSTRATIONFig. 1.—Divisions adopted for statistical discussion.
- ILLUSTRATIONFig. 2.—Shallow earthquakes, M ≥ 4, 1940-44.
- ILLUSTRATIONFig. 3.—Shallow earthquakes, M ≥ 4, 1945-49.
- ILLUSTRATIONFig. 4.—Shallow earthquakes, M ≥ 4, 1950-54.
- ILLUSTRATIONFig. 5.—Shallow earthquakes, M ≥ 4, 1955-59.
- ILLUSTRATIONFig. 6.—Shallow earthquakes, M ≥ 4, 1960-64.
- ILLUSTRATIONFig. 7.—Seismograph stations. WEL, Wellington; COB, Cobb River; KAI, Kaimata; CHR, Christchurch; GPZ, Gebbies Pass. E...
- ILLUSTRATIONFig. 8.—Histograms of earthquake frequency in the Regions identified in Fig. 1.
- ILLUSTRATIONFig. 9.—Number of shocks within 75km of the trend line between 1955 and 1964. The magnitude ranges have the stated fi...
- ILLUSTRATIONFig. 10.—Relation of the boundary between the Main and Central Seismic Regions to the Lord Howe Rise. Bathymetry from...
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