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14 Publications found! (Query time: 0.001 s) – Download as CSV file – Download as KML file

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Score ↓Exp/Site/HoleYearAuthor/TitleFull text
100%43
43-386		1983Lavoie, Dawn L.; Matthews, J. E.: Sediments on the southeastern flank of the Bermuda Pedestal
60%150
174A		2000McHugh, Cecilia M. G.; Damuth, John E. et al.: Late Pleistocene to Recent sedimentary activity on the New Jersey continental margin
25%49
49-410
49-412
49-413		1979Roberts, W. P.: Origin of basaltic gravelly sands, holes 410, 410A, 412A, and 413download
13%60
60-453		1982Natland, James H.: Petrography and mineral compositions of gabbros recovered in Deep Sea Drilling Project Hole 453 on the western side of the Mariana Troughdownload
13%144
144-873		1995Lincoln, Jonathan M.; Enos, Paul et al.: Stratigraphy and diagenesis of the carbonate platform at Site 873, Wodejebato Guyotdownload
13%1581998Petersen, Sven; Herzig, Peter M. et al.: Fluid inclusion studies as a guide to the temperature regime within the TAG hydrothermal mound, 26 degrees N, Mid-Atlantic Ridgedownload
10%95
95-612
95-613		1987Farre, J. A.; Ryan, W. B. F.: Surficial geology of the continental margin offshore New Jersey in the vicinity of Deep Sea Drilling Project sites 612 an 613download
10%106
106-649		1988Detrick, Robert S.; Honnorez, Jose et al.: Site 649download
10%144
144-874
144-875
144-876
144-877		1995Lincoln, Jonathan M.; Enos, Paul et al.: Geologic history of Wodejebato Guyotdownload
10%281975Hayes, D. E.; Frakes, L. A.: General synthesis, Deep Sea Drilling Project Leg 28download
9%1581998Hannington, Mark D.; Galley, Alan G. et al.: Comparison of the TAG mound and stockwork complex with cyprus-type massive sulfide depositsdownload
6%144
144-873		1993Premoli Silva, Isabella; Haggerty, Janet A. et al.: Site 873download
5%1181991Dick, Henry J. B.; Meyer, Peter S. et al.: Lithostratigraphic evolution of an in-situ section of oceanic layer 3download
1%121
121-758		2003Chen, Chang-Hwa; Ku, Y. P. et al.: The Toba Tuff in the Peninsula India; as a clue for the Acheulian puzzledownload

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