Zobrazeno 1 - 7
of 7
pro vyhledávání: '"M. D. Lilley"'
Autor:
C. R. German, T. Baumberger, M. D. Lilley, J. E. Lupton, A. E. Noble, M. Saito, A. R. Thurber, D. K. Blackman
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 3, Pp n/a-n/a (2022)
Abstract We report results from a hydrothermal plume survey along the southernmost Chile Rise from the Guamblin Fracture Zone to the Chile Triple Junction (CTJ) encompassing two segments (93 km cumulative length) of intermediate spreading‐rate mid
Externí odkaz:
https://doaj.org/article/43db6cb129b34d7dbfe7a2dac1f2aa54
Autor:
B. N. Orcutt, M. Bergenthal, T. Freudenthal, D. Smith, M. D. Lilley, L. Schnieders, S. Green, G. L. Früh-Green
Publikováno v:
Scientific Drilling, Vol 23, Pp 39-46 (2017)
IODP Expedition 357 utilized seabed drills for the first time in the history of the ocean drilling program, with the aim of collecting intact sequences of shallow mantle core from the Atlantis Massif to examine serpentinization processes and the d
Externí odkaz:
https://doaj.org/article/171defef09e244baaa18f4b4b3ebeba2
Autor:
M. D. Lilley, William S. D. Wilcock, David A. Butterfield, M. Summit, Deborah S. Kelley, J. R. Delaney, Robert W. Embley, J. A. Baross
Publikováno v:
Science. 281:222-230
Seafloor diking-eruptive events represent the irreducible, quantum events of upper oceanic crustal accretion. They record events by which a large portion of the oceanic crust has formed through geological history. Since 1993, the U.S. Navy's real-tim
Publikováno v:
Geological Society, London, Special Publications. 87:111-120
Dissolved concentrations of CH 4 , H 2 and Mn have been measured in a hydrothermal plume above the shallow water ( c. 250m) Steinaholl vent site at 63°N on the Reykjanes Ridge. Samples were taken in October 1990 and June 1993. In 1990 dissolved CH 4
Autor:
J R, Delaney, D S, Kelley, M D, Lilley, D A, Butterfield, J A, Baross, W S, Wilcock, R W, Embley, M, Summit
Publikováno v:
Science (New York, N.Y.). 281
Seafloor diking-eruptive events represent the irreducible, quantum events of upper oceanic crustal accretion. They record events by which a large portion of the oceanic crust has formed through geological history. Since 1993, the U.S. Navy's real-tim
Autor:
M. D. Lilley, J. F. Holden, R. E. McDuff, K. K. Roe, R. A. Feely, G. J. Massoth, J. R. Delaney, R. E. Embley, D. A. Butterfield, Ian R. Jonasson
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5d3cf6f8fe8c922aea0b453ba25ec1d4
https://doi.org/10.1017/cbo9780511600050.008
https://doi.org/10.1017/cbo9780511600050.008
Autor:
Delaney JR; J. R. Delaney, D. S. Kelley, M. D. Lilley, J. A. Baross, W. S. D. Wilcock, and M. Summit are at the School of Oceanography, University of Washington, Seattle, WA 98195, USA. D. A. Butterfield is at the Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration (NOAA), Seattle, WA 98115, USA. R. W. Embley is at the Pacific Marine Environmental Laboratory, NOAA, Newport, OR 97365, USA., Kelley DS, Lilley MD, Butterfield DA, Baross JA, Wilcock WSD, Embley RW, Summit M
Publikováno v:
Science (New York, N.Y.) [Science] 1998 Jul 10; Vol. 281 (5374), pp. 222-30.