New ocean crust is constantly being formed from mid-ocean ridge axis. Voluminous flows of lava are emplaced also away from the ridge axis, adding off-axis crustal layers to the crustal pile. Research on deep sea is of great importance to better understand the mechanisms and the nature of the crust forming and evolution. In this work, we decipher the first stages of the postmagmatic evolution of an intact volcanic section from the upper oceanic crust at ocean drilling program/integrated ocean drilling program (ODP/IODP) Site 1256 (Eastern Pacific Ocean). Using for the first time an innovative core-log integration technique to match direct (core-related) and indirect (borehole-related) data by depth shifting and reorienting individual core pi...
ODP Leg 203 established a new legacy hole for a long-term Dynamics of Earth and Ocean Systems/Ocean ...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
[1] The objective of this study is to construct a representative volcanostratigraphy of Ocean Drilli...
A complete ‘‘in situ’’ section of upper oceanic crust, from extrusive lavas, through dikes into gabb...
The igneous rocks cored in Holes 1256C and 1256D during Ocean Drilling Program (ODP) Leg 206 and Int...
ODP Leg 206 and IODP Expeditions 309/312 drilled a complete intact in situ section of the upper ocea...
This work examines a massive basaltic lava emplaced in a subaqueous environment and drilled at ODP S...
Ocean Drilling Program Site 1224 is located about halfway between California and Hawaii in the easte...
International audienceDuring the last decade, Integrated Ocean Drilling Program (IODP) has made subs...
The objective of this study is to construct a representative volcanostratigraphy of Ocean Drilling P...
The ocean crust is formed by the rising of magma from mid-ocean ridges and voluminous (1-30 km3) flo...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
ODP Leg 203 established a new legacy hole for a long-term Dynamics of Earth and Ocean Systems/Ocean ...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
ODP Leg 203 established a new legacy hole for a long-term Dynamics of Earth and Ocean Systems/Ocean ...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
[1] The objective of this study is to construct a representative volcanostratigraphy of Ocean Drilli...
A complete ‘‘in situ’’ section of upper oceanic crust, from extrusive lavas, through dikes into gabb...
The igneous rocks cored in Holes 1256C and 1256D during Ocean Drilling Program (ODP) Leg 206 and Int...
ODP Leg 206 and IODP Expeditions 309/312 drilled a complete intact in situ section of the upper ocea...
This work examines a massive basaltic lava emplaced in a subaqueous environment and drilled at ODP S...
Ocean Drilling Program Site 1224 is located about halfway between California and Hawaii in the easte...
International audienceDuring the last decade, Integrated Ocean Drilling Program (IODP) has made subs...
The objective of this study is to construct a representative volcanostratigraphy of Ocean Drilling P...
The ocean crust is formed by the rising of magma from mid-ocean ridges and voluminous (1-30 km3) flo...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
ODP Leg 203 established a new legacy hole for a long-term Dynamics of Earth and Ocean Systems/Ocean ...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
ODP Leg 203 established a new legacy hole for a long-term Dynamics of Earth and Ocean Systems/Ocean ...
International audienceThe distribution of faults and fault characteristics along the East Pacific Ri...
[1] The objective of this study is to construct a representative volcanostratigraphy of Ocean Drilli...