Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity

Gerhardt Einsele; Joris M. Gieskes; Joseph Curray; David M. Moore; Eduardo Aguayo; Marie Pierre Aubry; Daniel Fornari; José Guerrero; Miriam Kastner; Kerry Kelts; Mitchell Lyle; Yasumochi Matoba; Adolfo Molina-Cruz; Jeffrey Niemitz; Jaime Rueda; Andrew Saunders; Hans Schrader; Bernd Simoneit; Victor Vacquier

doi:10.1038/283441a0

Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity

Gerhardt Einsele, Joris M. Gieskes, Joseph Curray, David M. Moore, Eduardo Aguayo, Marie Pierre Aubry, Daniel Fornari, José Guerrero, Miriam Kastner, Kerry Kelts, Mitchell Lyle, Yasumochi Matoba, Adolfo Molina-Cruz, Jeffrey Niemitz, Jaime Rueda, Andrew Saunders, Hans Schrader, Bernd Simoneit, Victor Vacquier

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187 Citas (Scopus)

Resumen

Sill intrusions into highly porous sediments in the Guaymas Basin, Gulf of California, lead to low-grade metamorphism, thermal alteration and migration of organic compounds, marked changes in interstitial water chemistry, and large-scale expulsion of heated pore fluids. The latter process creates space for the intruding magma and initiates a hydrothermal system, which can explain the observed hydrothermal deposits around fault scarps on the basin floor.

Idioma original	Inglés
Páginas (desde-hasta)	441-445
Número de páginas	5
Publicación	Nature
Volumen	283
N.º	5746
DOI	https://doi.org/10.1038/283441a0
Estado	Publicada - 1980
Publicado de forma externa	Sí

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Einsele, G., Gieskes, J. M., Curray, J., Moore, D. M., Aguayo, E., Aubry, M. P., Fornari, D., Guerrero, J., Kastner, M., Kelts, K., Lyle, M., Matoba, Y., Molina-Cruz, A., Niemitz, J., Rueda, J., Saunders, A., Schrader, H., Simoneit, B., & Vacquier, V. (1980). Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity. Nature, 283(5746), 441-445. https://doi.org/10.1038/283441a0

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title = "Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity",

abstract = "Sill intrusions into highly porous sediments in the Guaymas Basin, Gulf of California, lead to low-grade metamorphism, thermal alteration and migration of organic compounds, marked changes in interstitial water chemistry, and large-scale expulsion of heated pore fluids. The latter process creates space for the intruding magma and initiates a hydrothermal system, which can explain the observed hydrothermal deposits around fault scarps on the basin floor.",

author = "Gerhardt Einsele and Gieskes, {Joris M.} and Joseph Curray and Moore, {David M.} and Eduardo Aguayo and Aubry, {Marie Pierre} and Daniel Fornari and Jos{\'e} Guerrero and Miriam Kastner and Kerry Kelts and Mitchell Lyle and Yasumochi Matoba and Adolfo Molina-Cruz and Jeffrey Niemitz and Jaime Rueda and Andrew Saunders and Hans Schrader and Bernd Simoneit and Victor Vacquier",

year = "1980",

doi = "10.1038/283441a0",

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pages = "441--445",

journal = "Nature",

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Einsele, G, Gieskes, JM, Curray, J, Moore, DM, Aguayo, E, Aubry, MP, Fornari, D, Guerrero, J, Kastner, M, Kelts, K, Lyle, M, Matoba, Y, Molina-Cruz, A, Niemitz, J, Rueda, J, Saunders, A, Schrader, H, Simoneit, B & Vacquier, V 1980, 'Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity', Nature, vol. 283, n.º 5746, pp. 441-445. https://doi.org/10.1038/283441a0

TY - JOUR

T1 - Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity

AU - Einsele, Gerhardt

AU - Gieskes, Joris M.

AU - Curray, Joseph

AU - Moore, David M.

AU - Aguayo, Eduardo

AU - Aubry, Marie Pierre

AU - Fornari, Daniel

AU - Guerrero, José

AU - Kastner, Miriam

AU - Kelts, Kerry

AU - Lyle, Mitchell

AU - Matoba, Yasumochi

AU - Molina-Cruz, Adolfo

AU - Niemitz, Jeffrey

AU - Rueda, Jaime

AU - Saunders, Andrew

AU - Schrader, Hans

AU - Simoneit, Bernd

AU - Vacquier, Victor

PY - 1980

Y1 - 1980

N2 - Sill intrusions into highly porous sediments in the Guaymas Basin, Gulf of California, lead to low-grade metamorphism, thermal alteration and migration of organic compounds, marked changes in interstitial water chemistry, and large-scale expulsion of heated pore fluids. The latter process creates space for the intruding magma and initiates a hydrothermal system, which can explain the observed hydrothermal deposits around fault scarps on the basin floor.

AB - Sill intrusions into highly porous sediments in the Guaymas Basin, Gulf of California, lead to low-grade metamorphism, thermal alteration and migration of organic compounds, marked changes in interstitial water chemistry, and large-scale expulsion of heated pore fluids. The latter process creates space for the intruding magma and initiates a hydrothermal system, which can explain the observed hydrothermal deposits around fault scarps on the basin floor.

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U2 - 10.1038/283441a0

DO - 10.1038/283441a0

M3 - Artículo

SN - 0028-0836

VL - 283

SP - 441

EP - 445

JO - Nature

JF - Nature

IS - 5746

ER -

Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity

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