Tectonic development

Takeuchi, A. (1980) Tertiary stress field and tectonic development of the southern part of the northeast Honshu Arc. J. Geosci. Osaka City U., 213, 1-64. 

Franz L., Brey G., and Okrusch M. (1996a) Steady state geotherm, thermal disturbances and tectonic development of the lower lithosphere underneath the Gibeon Kimberlite Province, Namibia. Contrib. Mineral. Petrol. 126, 181-198. 

Gabrielsen, R.H., 1984. Long-lived fault zones and their influence on the tectonic development of the south-western Barents Sea. J. Geol. Soc. London 141 651-662. 

Bukovics, C. Ziegler, P. A. 1985. Tectonic development of the Mid-Norway continental margin. Marine and Petroleum Geology, 2, 2-22. 

Weissbrod T, Perath I, Nachmias 1 (1987) Apatite as a Palaeoenvironmental indicator in the Precambrian-Mesozoic clastic sequence of the Middle East. J African Earth Sci 6 797-805 White SH, Green PF (1986) Tectonic development of the Alpine fault zone. New Zealand A fission track study. Geology 14 124-127... 

The eruption of the andesites observed in the central portion played an important role in the tectonic development of the province. Under the great weight of the sediments deposited in the depression, widespread fracturing developed around the periphery of the basins in the less stable zones which in turn aided the andesitic eruptions. The latter, as well as the Austrian orogeny, contributed to the modification of the shape of the basin. Its present appearance is the result of a long evolution starting at the end of the Paleozoic and lasting into the Tertiary. 

Sproli, K.B. 1980. New Zealand and oblique-slip margins Tectonic development up to and during the Cenozoic. In Sedimentation in Oblique-Slip Mobile Zones, Ballance, PP, and Reading, G.H., eds., International Association of Sedomentologists, Special Publication 4, pp. 147-170. 

On a larger scale, landscape development reflects those mechanisms that expose bedrock, weather it, and transport the weathering products away. Present and past tectonism, geology, climate, soils, and vegetation are all important to landscape evolution. These factors often operate in tandem to produce characteristic landforms that presumably integrate the effects of both episodic and continuous processes over considerable periods of time. 

Ronov, A. B., Migdisov, A. A., and Barskaya, N. V. (1969). Tectonic cycles and regularities in the development of sedimentary rocks and paleogeographic... 

Additional material on this subject is provided in the supplemental information for Chapter 25.4 that is available online at http //elsevierdirect.eom/companions/9780120885305. Key topics covered are the role of tectonism in the geologic carbon cycle and how the evolution of pelagic calcifiers in the Phanerozoic led to the development of feedbacks, some stabilizing and some destabilizing, that act on the atmospheric COj reservoir. Also included is a short summary of how the global carbon cycle interacts with the atmospheric O2 and sulfur cycles. 

Muffler, L. J. P. 1975. Tectonic and hydrologic control of the nature and distribution of geothermal resources. In Proceedings Second United Nations Symposium on the Development and Use of Geothermal Resources, San Francisco, 20-29 May 1975, 499-507. 

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