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- W197852433 abstract "Surficial joints are frequently grouped into three systems: two orthogonal systems that are approximately vertical (these are due to the neotectonic stress field) and one inclined system. The two vertical systems are divided by a smaller (maximum compression of σ 1 ) quadrant. In the Coastal Range of Venezuela we have measured the orientation of 635 joints, found in 10 groups of 3 outcrops each, located on three north-south profiles across the Coastal Range (Los Caracas-Caucagua, Matquetia-T a cata, and Puerto Colombia-G ϋ ig ῡ e) and occurring in Mesozoic rocks and in Quaternary sediments. In addition, in Curacao , 136 joints were measured in 6 outcrops in Quaternary reef limestone. The data were statistically evaluated according to the Kohlbeck-Scheidegger method. For the Coastal Range we obtained σ 1 : N130 ° E/06° and σ 3 : N80 ° E/O°, and there was no significant difference between σ 1 (and σ 3 ) in locations north and south of the La Victoria fault zone. For Curacao, σ 1 : N170 ° E/03°. The significant difference between the Coastal Range and Curacao suggests that the boundary between the Caribbean and South American plates is located north of the Venezuelan coast. The orientation of σ 1 in the Coastal Range conforms to other tectonic elements which indicate that the South American plate is moving to the northwest in relation to the Caribbean plate." @default.
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- W197852433 date "1986-04-11" @default.
- W197852433 modified "2023-09-24" @default.
- W197852433 title "Recent Joints and their Tectonic Significance in the Coastal Range of Venezuela and in Curacao" @default.
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