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Title: Banda-Celebes-Sulu basin - a trapped Cretaceous-Eocene oceanic crust

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6455911

The Banda, Celebes and Sulu Basins are three poorly understood marginal seas that are located at the junction of the Eurasian, Indian-Australian, Pacific and Philippine Sea plates. The incomplete data sets from each of these three marginal basins, the complex geological arrangement of the surrounding islands, and the compound late Cenozoic evolutions involving subduction, rifting, transform faulting and island arc collision have complicated any tectonic interpretations of this region. On the bases of marine geophysical data and on-land geology, the authors propose that the Banda, Celebes and Sulu Basins are the remanents of a once-continuous Cretaceous to Eocene ocean basin. Magnetic anomalies from the Banda, Celebes and Sulu Basins show the similar trends of about N70/sup 0/E, N60/sup 0/E and N55/sup 0/E respectively. Their best fit to the reversal models are as follows: (1) anomalies M1-M11 in the Banda Basin, (2) anomalies 30-33 in the Celebes Basin and (3) anomalies 17-20 in the Sulu Basin. The heat flow data from each of these basins is consistent with the relationship of our assigned magnetic ages. The on-land geology of this region is complicated by numerous land masses which dissect this old oceanic basin into the present configuration of marginal seas. The authors argue that each of these land masses arrived at its present location by either late Tertiary tectonic movements or has been built in place upon this older oceanic basement.

Research Organization:
Texas A and M Univ., College Station (USA)
OSTI ID:
6455911
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English