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  • 1
    Publication Date: 2023-02-08
    Description: Crustal properties of young oceanic lithosphere have been examined extensively, but the nature of the mantle lithosphere underneath remains elusive. Using a novel wide-angle seismic imaging technique, here we show the presence of two sub-horizontal reflections at ∼11 and ∼14.5 km below the seafloor over the 0.51–2.67 Ma old Juan de Fuca Plate. We find that the observed reflectors originate from 300–600-m-thick layers, with an ∼7–8% drop in P-wave velocity. They could be explained either by the presence of partially molten sills or frozen gabbroic sills. If partially molten, the shallower sill would define the base of a thin lithosphere with the constant thickness (11 km), requiring the presence of a mantle thermal anomaly extending up to 2.67 Ma. In contrast, if these reflections were frozen melt sills, they would imply the presence of thick young oceanic lithosphere (20–25 km), and extremely heterogeneous upper mantle.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 2
    Publication Date: 2023-02-08
    Description: Oceanic transform faults and fracture zones represent major bathymetric features that keep the records of past and present strike‐slip motion along conservative plate boundaries. Although they play an important role in ridge segmentation and evolution of the lithosphere, their structural characteristics, and their variation in space and time, are poorly understood. To address some of the unknowns, we conducted interdisciplinary geophysical studies in the equatorial Atlantic Ocean, the region where some of the most prominent transform discontinuities have been developing. Here we present the results of the data analysis in the vicinity of the Chain Fracture Zone (FZ), on the South American Plate. The crustal structure across the Chain FZ, at the contact between ~10 and 24 Ma oceanic lithosphere, is sampled along seismic reflection and refraction profiles. We observe that the crustal thickness within and across the Chain FZ ranges from ~4.6‐5.9 km, which compares with the observations reported for slow‐slipping transform discontinuities globally. We attribute this presence of close to normal oceanic crustal thickness within fracture zones to the mechanism of lateral dike propagation, previously considered to be valid only in fast‐slipping environments. Furthermore, the combination of our results with other datasets enabled us to extend the observations to morpho‐tectonic characteristics on a regional scale. Our broader view suggests that the formation of the transverse ridge is closely associated with a global plate reorientation that was also responsible for the propagation and for shaping lower‐order Mid‐Atlantic Ridge segmentation around the equator.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 3
    Publication Date: 2024-02-07
    Description: Plate tectonics characterize transform faults as conservative plate boundaries where the lithosphere is neither created nor destroyed. In the Atlantic, both transform faults and their inactive traces, fracture zones, are interpreted to be structurally heterogeneous, representing thin, intensely fractured, and hydrothermally altered basaltic crust overlying serpentinized mantle. This view, however, has recently been challenged. Instead, transform zone crust might be magmatically augmented at ridge-transform intersections before becoming a fracture zone. Here, we present constraints on the structure of oceanic crust from seismic refraction and wide-angle data obtained along and across the St. Paul fracture zone near 18°W in the equatorial Atlantic Ocean. Most notably, both crust along the fracture zone and away from it shows an almost uniform thickness of 5-6 km, closely resembling normal oceanic crust. Further, a well-defined upper mantle refraction branch supports a normal mantle velocity of 8 km/s along the fracture zone valley. Therefore, the St. Paul fracture zone reflects magmatically accreted crust instead of the anomalous hydrated lithosphere. Little variation in crustal thickness and velocity structure along a 200 km long section across the fracture zone suggests that distance to a transform fault had negligible impact on crustal accretion. Alternatively, it could also indicate that a second phase of magmatic accretion at the proximal ridge-transform intersection overprinted features of starved magma supply occurring along transform faults. Key Points: - Seismic structure along the St. Paul fracture zone reflects magmatically accreted oceanic crust - Oceanic crust across St. Paul shows only small thickness variations, lacking evidence for regional crustal thinning near fracture zones - Magmatic nature of crust supports a mechanism where transform crust is augmented before being turned into a fracture zone
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: other
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  • 4
    Publication Date: 2023-08-24
    Description: We provide a processed gravity (Free-air anomaly) dataset collected in the equatorial Atlantic during ILAB-SPARC experiment conducted aboard N/O Pourquoi Pas? in Fall 2018.
    Keywords: Equatorial Atlantic; Free-air gravity anomaly; GRAV; Gravimeter (Bondenseewerk KSS31); Gravimetry; gravity; ILAB-SPARC; ILAB-SPARC_Profile1A; LATITUDE; LONGITUDE; Pourquoi Pas ? (2005)
    Type: Dataset
    Format: text/tab-separated-values, 74992 data points
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  • 5
    Publication Date: 2024-04-20
    Description: We provide processed bathymetry and gravity (Free-air anomaly) datasets collected in the equatorial Atlantic during ILAB-SPARC experiment conducted aboard N/O Pourquoi Pas? in Fall 2018. The seismic data sample the oceanic lithosphere extending between the Romanche Transform Fault to the Charcot Fracture Zone. Refraction data were collected during the ILAB-SPARC experiment. The provided refraction data were recorded on 25 Ocean Bottom Seismometer (OBS data) instruments (from 25 to 50) and span source-receiver offsets from ~-100 km to 100 km. Reflection (multichannel seismic - MCS data), we provide are sorted as CMP gathers that were used to produce seismic sections for imaging layer 2A. The data were collected during two experiments, using different survey geometries: 1) ILAB_SPARC_CMP.segy (in 5 parts): collected during ILAB_SPARC experiment in 2018, sample the region south of the Chain Fracture Zone. The maximum source-receiver offset is ~6 km. Note that the provided data were interpolated only in the shot domain (data fold 40). 2) TransAtlantic_CMP.segy (provided in two parts): collected during iLAB TransAtlantic survey aboard M/V Western Trident in Spring 2015. The data sample the region between the Chain Fracture ZOne and Romanche Transform Fault. The maximum source-receiver offset provided is ~ 6 km. Finally, we provide our final velocity model obtained by analyzing the OBS data (the data are provided in ascii format (horizontal and vertical grid sizes are 200 m and 50 m, respectively).
    Keywords: Bathymetry; Equatorial Atlantic; gravity; MCS seismic; OBS
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 6
    Publication Date: 2024-04-20
    Description: We provide a processed bathymetry dataset collected in the equatorial Atlantic during ILAB-SPARC experiment conducted aboard N/O Pourquoi Pas? in Fall 2018.
    Keywords: Bathymetry; Equatorial Atlantic; ILAB-SPARC; ILAB-SPARC_MB; MB; Multibeam; Pourquoi Pas ? (2005)
    Type: Dataset
    Format: application/x-netcdf, 247 MBytes
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  • 7
    Publication Date: 2024-04-20
    Description: The seismic data sample the oceanic lithosphere extending between the Romanche Transform Fault to the Charcot Fracture Zone. Reflection (multichannel seismic - MCS data), we provide are sorted as CMP gathers that were used to produce seismic sections for imaging layer 2A. The data were collected during two experiments, using different survey geometries: 1) ILAB_SPARC_CMP.segy (in 5 parts): collected during ILAB_SPARC experiment conducted aboard N/O Pourquoi Pas? in Fall 2018, sample the region south of the Chain Fracture Zone. The maximum source-receiver offset is ~6 km. Note that the provided data were interpolated only in the shot domain (data fold 40). 2) TransAtlantic_CMP.segy (provided in two parts): collected during iLAB TransAtlantic survey aboard M/V Western Trident in Spring 2015. The data sample the region between the Chain Fracture ZOne and Romanche Transform Fault. The maximum source-receiver offset provided is ~ 6 km.
    Keywords: Binary Object; Equatorial Atlantic; Event label; File content; ILAB-SPARC; ILAB-SPARC-track; iLAB-TransAtlantic; iLAB-TransAtlantic-track; MCSEIS; MCS seismic; Multichannel seismics; Pourquoi Pas ? (2005); Western Trident
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 8
    Publication Date: 2024-04-20
    Description: These dataset was collected in the equatorial Atlantic during ILAB-SPARC experiment conducted aboard N/O Pourquoi Pas? in Fall 2018. The seismic data sample the oceanic lithosphere extending between the Romanche Transform Fault to the Charcot Fracture Zone. Refraction data were collected during the ILAB-SPARC experiment. The provided refraction data were recorded on 25 Ocean Bottom Seismometer (OBS data) instruments (from 25 to 50) and span source-receiver offsets from ~-100 km to 100 km. Finally, we provide our final velocity model obtained by analyzing the OBS data (the data are provided in ascii format (horizontal and vertical grid sizes are 200 m and 50 m, respectively).
    Keywords: Binary Object; Binary Object (File Size); Equatorial Atlantic; Event label; ILAB-SPARC; ILAB-SPARC_OBS_26; ILAB-SPARC_OBS_27; ILAB-SPARC_OBS_28; ILAB-SPARC_OBS_29; ILAB-SPARC_OBS_30; ILAB-SPARC_OBS_31; ILAB-SPARC_OBS_32; ILAB-SPARC_OBS_33; ILAB-SPARC_OBS_34; ILAB-SPARC_OBS_35; ILAB-SPARC_OBS_36; ILAB-SPARC_OBS_37; ILAB-SPARC_OBS_38; ILAB-SPARC_OBS_39; ILAB-SPARC_OBS_40; ILAB-SPARC_OBS_41; ILAB-SPARC_OBS_42; ILAB-SPARC_OBS_43; ILAB-SPARC_OBS_44; ILAB-SPARC_OBS_45; ILAB-SPARC_OBS_46; ILAB-SPARC_OBS_47; ILAB-SPARC_OBS_48; ILAB-SPARC_OBS_49; ILAB-SPARC_OBS_50; OBS; Ocean bottom seismometer; Pourquoi Pas ? (2005)
    Type: Dataset
    Format: text/tab-separated-values, 26 data points
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  • 9
    Publication Date: 2024-04-20
    Description: The provided data are pre-stack depth (psdm) and pre-stack time (pstm) migrated Ocean Bottom Hydrophone datasets for the lines RFR96-01, RFR96-03, RFR96-05, and RFR96-08. In addition to seismic data, the picks of the shallowest and deepest events are provided.
    Keywords: Binary Object; Binary Object (File Size); Event label; HYDROCELL; migration; North Pacific Ocean; picks; pre-stack depth migrated; pre-stack time migrated; Seismic refraction profile; SEISREFR; SO111; SO111_RFR96-01; SO111_RFR96-03; SO111_RFR96-05; SO111_RFR96-08; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2011. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry Geophysics Geosystems 12 (2011): Q05008, doi:10.1029/2010GC003439.
    Description: Variations in topography and seismic structure are observed along the Juan de Fuca (JdF) Ridge axis and in the vicinity of pseudofaults on the ridge flanks left by former episodes of ridge propagation. Here we analyze gravity data coregistered with multichannel seismic data from the JdF Ridge and flanks in order to better understand the origin of crustal structure variations in this area. The data were collected along the ridge axis and along three ridge-perpendicular transects at the Endeavor, Northern Symmetric, and Cleft segments. Negative Mantle Bouguer anomalies of −21 to −28 mGal are observed at the axis of the three segments. Thicker crust at the Endeavor and Cleft segments is inferred from seismic data and can account for the small differences in axial gravity anomalies (3–7 mGal). Additional low densities/elevated temperatures within and/or below the axial crust are required to explain the remaining axial MBA low at all segments. Gravity models indicate that the region of low densities is wider beneath the Cleft segment. Gravity models for pseudofaults crossed along the three transects support the presence of thinner and denser crust within the pseudofault zones that we attribute to iron-enriched crust. On the young crust side of the pseudofaults, a 10–20 km wide zone of thicker crust is found. Reflection events interpreted as subcrustal sills underlie the zones of thicker crust and are the presumed source for the iron enrichment.
    Description: This work was supported by the National Science Foundation grants OCE‐0648303 to Lamont‐Doherty Earth Observatory, OCE‐0648923 to Woods Hole Oceanographic Institution.
    Keywords: Mid-ocean ridges ; Propagation ; Juan de Fuca Ridge ; Gravity
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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