Skip to main content

Research Repository

Advanced Search

Outputs (157)

Vp/Vs structure and Pn anisotropy across the Louisville Ridge, seaward of the Tonga-Kermadec Trench (2024)
Journal Article
Contreras-Reyes, E., Grevemeyer, I., Peirce, C., & Obando-Orrego, S. (2024). Vp/Vs structure and Pn anisotropy across the Louisville Ridge, seaward of the Tonga-Kermadec Trench. Tectonophysics, 885, Article 230417. https://doi.org/10.1016/j.tecto.2024.230417

The Pacific Plate within the collision zone between the Louisville Ridge and the Tonga-Kermadec Trench was formed at the Osbourn Trough, a paleo spreading center that became inactive during the Cretaceous. In this region, the trench shallows from a d... Read More about Vp/Vs structure and Pn anisotropy across the Louisville Ridge, seaward of the Tonga-Kermadec Trench.

Application of a seismic network to baleen whale call detection and localization in the Panama basin-a Bryde's whale example. (2024)
Journal Article
Tary, J. B., Peirce, C., Hobbs, R., Bonilla Walker, F., De La Hoz, C., Bird, A., & Vargas, C. A. (2024). Application of a seismic network to baleen whale call detection and localization in the Panama basin-a Bryde's whale example. The Journal of the Acoustical Society of America, 155(3), 2075-2086. https://doi.org/10.1121/10.0025290

Baleen whales use sounds of various characteristics for different tasks and interactions. This study focuses on recordings from the Costa Rica Rift, in the Eastern Tropical Pacific Ocean, made by 25 ocean-bottom seismographs and a vertical array of 1... Read More about Application of a seismic network to baleen whale call detection and localization in the Panama basin-a Bryde's whale example..

Oceanic crust – seismic structure, lithology and the cause of the 2A Event at borehole 504B (2024)
Journal Article
Peirce, C., & Hobbs, R. (2024). Oceanic crust – seismic structure, lithology and the cause of the 2A Event at borehole 504B. Geophysical Journal International, 237(1), 159-189. https://doi.org/10.1093/gji/ggae029

This study focuses on the 3-D velocity structure and thickness of ~7 Myr-old oceanic crust surrounding borehole 504B, located ~235 km from the intermediate-spreading Costa Rica Rift (Panama Basin). It investigates how well seismic structure determine... Read More about Oceanic crust – seismic structure, lithology and the cause of the 2A Event at borehole 504B.

Structure and dynamics of the Ecuador Fracture Zone, Panama Basin (2023)
Journal Article
Peirce, C., Tedd, J., & Hobbs, R. (2023). Structure and dynamics of the Ecuador Fracture Zone, Panama Basin. Geophysical Journal International, 235(2), 1519-1540. https://doi.org/10.1093/gji/ggad315

In this study, multiple geophysical data types are used to investigate the structure and dynamics of the Ecuador Fracture Zone – a complex multi-stranded strike-slip fault system located in the Panama Basin. Gravity modelling reveals a 25-30 km-wide... Read More about Structure and dynamics of the Ecuador Fracture Zone, Panama Basin.

Three-dimensional S-wave velocity structure of oceanic core complexes at 13N on the Mid-Atlantic Ridge (2022)
Journal Article
Peirce, C., Funnell, M., Reston, T., & MacLeod, C. (2022). Three-dimensional S-wave velocity structure of oceanic core complexes at 13N on the Mid-Atlantic Ridge. Geophysical Journal International, 232(1), 615-642. https://doi.org/10.1093/gji/ggac350

13°N on the Mid-Atlantic Ridge is regarded as a type site for oceanic core complexes (OCCs). Within ~70 km along the spreading centre, it hosts four OCCs in different stages of their life cycle making this an ideal location to determine how OCCs are... Read More about Three-dimensional S-wave velocity structure of oceanic core complexes at 13N on the Mid-Atlantic Ridge.

Carbon and sediment fluxes inhibited in the submarine Congo Canyon by landslide-damming (2022)
Journal Article
Pope, E. L., Heijnen, M. S., Talling, P. J., Jacinto, R. S., Gaillot, A., Baker, M. L., …Urlaub, M. (2022). Carbon and sediment fluxes inhibited in the submarine Congo Canyon by landslide-damming. Nature Geoscience, 15(10), 845-853. https://doi.org/10.1038/s41561-022-01017-x

Landslide-dams, which are often transient, can strongly affect the geomorphology, and sediment and geochemical fluxes, within subaerial fluvial systems. The potential occurrence and impact of analogous landslide-dams in submarine canyons has, however... Read More about Carbon and sediment fluxes inhibited in the submarine Congo Canyon by landslide-damming.

Longest sediment flows yet measured show how major rivers connect efficiently to deep sea (2022)
Journal Article
Talling, P. J., Baker, M. L., Pope, E. L., Ruffell, S. C., Jacinto, R. S., Heijnen, M. S., …Hilton, R. J. (2022). Longest sediment flows yet measured show how major rivers connect efficiently to deep sea. Nature Communications, 13(1), https://doi.org/10.1038/s41467-022-31689-3

Here we show how major rivers can efficiently connect to the deep-sea, by analysing the longest runout sediment flows (of any type) yet measured in action on Earth. These seafloor turbidity currents originated from the Congo River-mouth, with one flo... Read More about Longest sediment flows yet measured show how major rivers connect efficiently to deep sea.

Active ocean-continent transform margins: seismic investigation of the Cayman Trough-Swan Island ridge-transform intersection (2022)
Journal Article
Peirce, C., Grevemeyer, I., Hayman, N., & Van Avendonk, H. (2022). Active ocean-continent transform margins: seismic investigation of the Cayman Trough-Swan Island ridge-transform intersection. Geophysical Journal International, 229(3), 1604-1627. https://doi.org/10.1093/gji/ggac019

The southern boundary of the Cayman Trough in theCaribbean is marked by the Swan Islands transform fault (SITF), which also represents the ocean-continent transition of the Honduras continental margin. This is one of the few places globally where a t... Read More about Active ocean-continent transform margins: seismic investigation of the Cayman Trough-Swan Island ridge-transform intersection.

Local rift and intraplate seismicity reveal shallow crustal fluid-related activity and sub-crustal faulting (2021)
Journal Article
Tary, J., Hobbs, R., Peirce, C., Lesmes Lesmes, C., & Funnell, M. (2021). Local rift and intraplate seismicity reveal shallow crustal fluid-related activity and sub-crustal faulting. Earth and Planetary Science Letters, 562, Article 116857. https://doi.org/10.1016/j.epsl.2021.116857

Seismicity delineating the mid-ocean ridge system in the Panama Basin is mostly concentrated along transform offsets. Most intraplate areas show little-to-no seismic activity. Here we analyze passive recordings from a short-term deployment of 75 ocea... Read More about Local rift and intraplate seismicity reveal shallow crustal fluid-related activity and sub-crustal faulting.

Evolution and properties of young oceanic crust: constraints from Poisson's ratio (2021)
Journal Article
Funnell, M., Robinson, A., Hobbs, R., & Peirce, C. (2021). Evolution and properties of young oceanic crust: constraints from Poisson's ratio. Geophysical Journal International, 225(3), 1874-1896. https://doi.org/10.1093/gji/ggab062

The seismic velocity of the oceanic crust is a function of its physical properties that include its lithology, degree of alteration, and porosity. Variations in these properties are particularly significant in young crust, but also occur with age as... Read More about Evolution and properties of young oceanic crust: constraints from Poisson's ratio.

Seismicity trends and detachment fault structure at 13N, Mid-Atlantic Ridge (2020)
Journal Article
Parnell-Turner, R., Sohn, R., Peirce, C., Reston, R., MacLeod, C., Searle, R., & Simao, N. (2021). Seismicity trends and detachment fault structure at 13N, Mid-Atlantic Ridge. Geology, 49(3), 320-324. https://doi.org/10.1130/g48420.1

At slow-spreading ridges, plate separation is commonly partly accommodated by slip on long-lived detachment faults, exposing upper mantle and lower crustal rocks on the seafloor. However, the mechanics of this process, the subsurface structure, and t... Read More about Seismicity trends and detachment fault structure at 13N, Mid-Atlantic Ridge.

Magmatic and tectonic segmentation of the intermediate-spreading Costa Rica Rift - a fine balance between magma supply rate, faulting, and hydrothermal circulation (2020)
Journal Article
Robinson, A., Zhang, L., Hobbs, R., Peirce, C., & Tong, V. (2020). Magmatic and tectonic segmentation of the intermediate-spreading Costa Rica Rift - a fine balance between magma supply rate, faulting, and hydrothermal circulation. Geophysical Journal International, 222(1), 132-152. https://doi.org/10.1093/gji/ggaa152

3-D tomographic modelling of wide-angle seismic data, recorded at the intermediate-spreading Costa Rica Rift, has revealed a P-wave seismic velocity anomaly low located beneath a small overlapping spreading centre that forms a non-transform discontin... Read More about Magmatic and tectonic segmentation of the intermediate-spreading Costa Rica Rift - a fine balance between magma supply rate, faulting, and hydrothermal circulation.

3-D P-wave velocity structure of oceanic core complexes at 13◦N on the Mid-Atlantic Ridge (2020)
Journal Article
Simão, N., Peirce, C., Funnell, M., Robinson, A., Searle, R., MacLeod, C., & Reston, T. (2020). 3-D P-wave velocity structure of oceanic core complexes at 13◦N on the Mid-Atlantic Ridge. Geophysical Journal International, 221(3), 1555-1579. https://doi.org/10.1093/gji/ggaa093

The Mid-Atlantic Ridge at 13° N is regarded as a type locality for oceanic core complexes (OCCs), as it contains, within ∼70 km along the spreading axis, four that are at different stages of their life cycle. The wealth of existing seabed observation... Read More about 3-D P-wave velocity structure of oceanic core complexes at 13◦N on the Mid-Atlantic Ridge.

Magmatism versus serpentinization – crustal structure along the 13°N segment at the Mid-Atlantic Ridge (2020)
Journal Article
Peirce, C., Robinson, A., Funnell, M., Searle, R., MacLeod, C., & Reston, T. (2020). Magmatism versus serpentinization – crustal structure along the 13°N segment at the Mid-Atlantic Ridge. Geophysical Journal International, 221(2), 981-1001. https://doi.org/10.1093/gji/ggaa052

A region of oceanic core complexes (OCCs) exists at 13°N on the Mid-Atlantic Ridge that is regarded as a type site. This site includes two OCCs at 13°20′N and 13°30′N, thought to be in the active and dying stages of evolution, and two together called... Read More about Magmatism versus serpentinization – crustal structure along the 13°N segment at the Mid-Atlantic Ridge.

Magma-hydrothermal interactions at the Costa Rica Rift from data collected in 1994 and 2015 (2019)
Journal Article
Lowell, R., Zhang, L., Maqueda, M., Banyte, D., Tong, V., Johnston, R., …Robinson, A. (2020). Magma-hydrothermal interactions at the Costa Rica Rift from data collected in 1994 and 2015. Earth and Planetary Science Letters, 531, Article 115991. https://doi.org/10.1016/j.epsl.2019.115991

We use co-located CTD/transmissometry casts and multichannel seismic reflection surveys conducted at the Costa Rica Rift (CRR) to provide a better understanding of magma-hydrothermal processes occurring at an intermediate-rate spreading center. Water... Read More about Magma-hydrothermal interactions at the Costa Rica Rift from data collected in 1994 and 2015.

Constraining the maximum depth of brittle deformation at slow- and ultraslow-spreading ridges using microseismicity (2019)
Journal Article
Grevemeyer, I., Hayman, N., Lange, D., Peirce, C., Papenberg, C., Van Avendonk, H., …Dannowski, A. (2019). Constraining the maximum depth of brittle deformation at slow- and ultraslow-spreading ridges using microseismicity. Geology, 47(11), 1069-1073. https://doi.org/10.1130/g46577.1

The depth of earthquakes along mid-ocean ridges is restricted by the relatively thin brittle lithosphere that overlies a hot, upwelling mantle. With decreasing spreading rate, earthquakes may occur deeper in the lithosphere, accommodating strain with... Read More about Constraining the maximum depth of brittle deformation at slow- and ultraslow-spreading ridges using microseismicity.

Seismic investigation of an active ocean-continent transform margin: the interaction between the Swan Islands Fault Zone and the ultraslow-spreading Mid-Cayman Spreading Centre (2019)
Journal Article
Peirce, C., Robinson, A., Campbell, A., Funnell, M., Grevemeyer, I., Hayman, N., …Castiello, G. (2019). Seismic investigation of an active ocean-continent transform margin: the interaction between the Swan Islands Fault Zone and the ultraslow-spreading Mid-Cayman Spreading Centre. Geophysical Journal International, 219(1), 159-184. https://doi.org/10.1093/gji/ggz283

Does intermediate spreading-rate oceanic crust result from episodic transition between magmatic and magma-dominated, faulting-enhanced spreading? – the Costa Rica Rift example (2019)
Journal Article
Wilson, D., Robinson, A., Hobbs, R., Peirce, C., & Funnell, M. (2019). Does intermediate spreading-rate oceanic crust result from episodic transition between magmatic and magma-dominated, faulting-enhanced spreading? – the Costa Rica Rift example. Geophysical Journal International, 218(3), 1617-1641. https://doi.org/10.1093/gji/ggz184

Ocean-bottom seismograph and multichannel streamer wide-angle seismic data are jointly analysed and compared with reflection images, bathymetric maps and potential field data, to reveal the detailed structure of layer 2 of the oceanic crust formed at... Read More about Does intermediate spreading-rate oceanic crust result from episodic transition between magmatic and magma-dominated, faulting-enhanced spreading? – the Costa Rica Rift example.

Constraints on crustal structure of adjacent OCCs and segment boundaries at 13N on the Mid-Atlantic Ridge (2019)
Journal Article
Peirce, C., Reveley, G., Simao, N., Robinson, A., Funnell, M., Searle, R., …Reston, T. (2019). Constraints on crustal structure of adjacent OCCs and segment boundaries at 13N on the Mid-Atlantic Ridge. Geophysical Journal International, 217(2), 988-1010. https://doi.org/10.1093/gji/ggz074

The 13° N segment of the Mid-Atlantic Ridge is an example of a morphologically well-studied slow spreading ridge segment populated with oceanic core complexes (OCCs). In this paper we present the results of a ∼200 km-long 2D seismic and gravity trans... Read More about Constraints on crustal structure of adjacent OCCs and segment boundaries at 13N on the Mid-Atlantic Ridge.

The Mid-Atlantic Ridge near 13º20’N: High-Resolution Magnetic and Bathymetry Imaging (2018)
Journal Article
Searle, R., MacLeod, C., Peirce, C., & Reston, T. (2019). The Mid-Atlantic Ridge near 13º20’N: High-Resolution Magnetic and Bathymetry Imaging. Geochemistry, Geophysics, Geosystems, 20(1), 295-313. https://doi.org/10.1029/2018gc007940

We describe detailed magnetic and bathymetric studies around 13°N on the Mid‐Atlantic Ridge, a site of extensive detachment faulting. Inversion of closely spaced sea surface magnetic anomalies reveals a disorganized pattern of magnetization, with ano... Read More about The Mid-Atlantic Ridge near 13º20’N: High-Resolution Magnetic and Bathymetry Imaging.

Construction and subduction of the Louisville Ridge, SW Pacific—insights from wide-angle seismic data modelling (2018)
Journal Article
Robinson, A., Peirce, C., & Funnell, M. (2018). Construction and subduction of the Louisville Ridge, SW Pacific—insights from wide-angle seismic data modelling. Geophysical Journal International, 215(3), 2222-2245. https://doi.org/10.1093/gji/ggy397

The Louisville Ridge is a ca. 4000 km-long chain of seamounts in the SW Pacific that is currently being subducted at the Tonga-Kermadec trench. The Pacific Plate, on which the chain sits, is subducting obliquely beneath the Indo-Australian Plate. Com... Read More about Construction and subduction of the Louisville Ridge, SW Pacific—insights from wide-angle seismic data modelling.

Episodic magmatism and serpentinized mantle exhumation at an ultraslow spreading centre (2018)
Journal Article
Grevemeyer, I., Hayman, N., Peirce, C., Schwardt, M., van Avendonk, H., Dannowski, A., & Papenberg, C. (2018). Episodic magmatism and serpentinized mantle exhumation at an ultraslow spreading centre. Nature Geoscience, 11, 444-448. https://doi.org/10.1038/s41561-018-0124-6

Mid-ocean ridges spreading at ultraslow rates of less than 20 mm yr−1 can exhume serpentinized mantle to the seafloor, or they can produce magmatic crust. However, seismic imaging of ultraslow-spreading centres has not been able to resolve the abunda... Read More about Episodic magmatism and serpentinized mantle exhumation at an ultraslow spreading centre.

Determining the extent of hydrothermal interaction on the southern Costa Rica Rift ridge flank during the past 8 Ma from joint inversion of geophysical data (2017)
Presentation / Conference Contribution
Wilson, D., Moorkamp, M., Hobbs, R., Peirce, C., Harris, R., & Morgan, J. (2017, December). Determining the extent of hydrothermal interaction on the southern Costa Rica Rift ridge flank during the past 8 Ma from joint inversion of geophysical data. Paper presented at American Geophysical Union Fall Meeting

Oceanic detachment faults generate compression in extension (2017)
Journal Article
Parnell-Turner, R., Sohn, R., Peirce, C., Reston, T., MacLeod, C., Searle, R., & Simão, N. (2017). Oceanic detachment faults generate compression in extension. Geology, 45(10), 923-926. https://doi.org/10.1130/g39232.1

In extensional geologic systems such as mid-ocean ridges, deformation is typically accommodated by slip on normal faults, where material is pulled apart under tension and stress is released by rupture during earthquakes and magmatic accretion. Howeve... Read More about Oceanic detachment faults generate compression in extension.

Magmatic-tectonic conditions for hydrothermal venting on an ultraslow-spread oceanic core complex (2017)
Journal Article
Harding, J., Van Avendonk, H., Hayman, N., Grevemeyer, I., Peirce, C., & Dannowski, A. (2017). Magmatic-tectonic conditions for hydrothermal venting on an ultraslow-spread oceanic core complex. Geology, 45(9), 839-842. https://doi.org/10.1130/g39045.1

Hydrothermal venting, an important cooling mechanism of the Earth, supports a diverse array of seafloor and sub-seafloor ecosystems that are sustained by large thermal and chemical fluxes. Vents have been found along even the slowest and coldest spre... Read More about Magmatic-tectonic conditions for hydrothermal venting on an ultraslow-spread oceanic core complex.

Seismic structure and segmentation of the axial valley of the Mid-Cayman Spreading Center (2017)
Journal Article
Van Avendonk, H., Hayman, N., Harding, J., Grevemeyer, I., Peirce, C., & Dannowski, A. (2017). Seismic structure and segmentation of the axial valley of the Mid-Cayman Spreading Center. Geochemistry, Geophysics, Geosystems, 18(6), 2149-2161. https://doi.org/10.1002/2017gc006873

We report the results of a two-dimensional tomographic inversion of marine seismic refraction data from an array of ocean-bottom seismographs (OBSs), which produced an image of the crustal structure along the axial valley of the ultraslow-spreading M... Read More about Seismic structure and segmentation of the axial valley of the Mid-Cayman Spreading Center.

Structural variability of the Tonga-Kermadec forearc characterised using robustly constrained geophysical data (2017)
Journal Article
Funnell, M., Peirce, C., & Robinson, A. (2017). Structural variability of the Tonga-Kermadec forearc characterised using robustly constrained geophysical data. Geophysical Journal International, 210(3), 1681-1702. https://doi.org/10.1093/gji/ggx260

Subducting bathymetric anomalies enhance erosion of the overriding forearc crust. The deformation associated with this process is superimposed on pre-existing variable crustal and sedimentary structures developed as a subduction system evolves. Recen... Read More about Structural variability of the Tonga-Kermadec forearc characterised using robustly constrained geophysical data.

Research and Outreach at the Mid-Atlantic Ridge (2016)
Journal Article
Searle, R., Peirce, C., & Bentley, A. (2016). Research and Outreach at the Mid-Atlantic Ridge. Astronomy and Geophysics, 57(3), 3.18-3.20. https://doi.org/10.1093/astrogeo/atw098

Roger Searle, Christine Peirce and Angela Bentley look at research on oceanic core complexes and detachments at the Mid-Atlantic Ridge, combined with innovative geophysics outreach.

Seismic velocity structure and deformation due to collision of the Louisville Ridge with the Tonga-Kermadec Trench (2015)
Journal Article
Stratford, W., Peirce, C., Funnell, M., Paulatto, M., Watts, A., Grevemeyer, I., & Bassett, D. (2015). Seismic velocity structure and deformation due to collision of the Louisville Ridge with the Tonga-Kermadec Trench. Geophysical Journal International, 200(3), 1503-1522. https://doi.org/10.1093/gji/ggu475

New marine geophysical data recorded across the Tonga-Kermadec subduction zone are used to image deformation and seismic velocity structures of the forearc and Pacific Plate where the Louisville Ridge seamount chain subducts. Due to the obliquity of... Read More about Seismic velocity structure and deformation due to collision of the Louisville Ridge with the Tonga-Kermadec Trench.

Structure and deformation of the Kermadec forearc in response to subduction of the Pacific oceanic plate (2014)
Journal Article
Funnell, M., Peirce, C., Stratford, W., Paulatto, M., Watts, A., & Grevemeyer, I. (2014). Structure and deformation of the Kermadec forearc in response to subduction of the Pacific oceanic plate. Geophysical Journal International, 199(2), 1286-1302. https://doi.org/10.1093/gji/ggu330

The Tonga-Kermadec forearc is deforming in response to on-going subduction of the Pacific Plate beneath the Indo-Australian Plate. Previous research has focussed on the structural development of the forearc where large bathymetric features such as th... Read More about Structure and deformation of the Kermadec forearc in response to subduction of the Pacific oceanic plate.

Potential field and bathymetric investigation of the Monowai volcanic centre, Kermadec arc: implications for caldera formation and volcanic evolution (2014)
Journal Article
Paulatto, M., Watts, A., & Peirce, C. (2014). Potential field and bathymetric investigation of the Monowai volcanic centre, Kermadec arc: implications for caldera formation and volcanic evolution. Geophysical Journal International, 197(3), 1484-1499. https://doi.org/10.1093/gji/ggt512

The dynamics of caldera formation are affected by internal factors, such as magma chamber structure and properties and regional tectonic stresses. Understanding their interrelationship is important for assessing volcanic hazard and reconstructing the... Read More about Potential field and bathymetric investigation of the Monowai volcanic centre, Kermadec arc: implications for caldera formation and volcanic evolution.

Uplift at lithospheric swells – II: is the Cape Verde mid-plate swell supported by a lithosphere of varying mechanical strength? (2013)
Journal Article
Wilson, D., Peirce, C., Watts, A., & Grevemeyer, I. (2013). Uplift at lithospheric swells – II: is the Cape Verde mid-plate swell supported by a lithosphere of varying mechanical strength?. Geophysical Journal International, 193(2), 798-819. https://doi.org/10.1093/gji/ggt034

The Cape Verde mid-plate swell is the largest amplitude oceanic mid-plate swell on Earth at ∼1800 km in diameter, with a crest ∼2.2 km high, and long-wavelength positive geoid, gravity and heat flow anomalies of 8 m, 30 mGal and 10–15 mW m−2, respect... Read More about Uplift at lithospheric swells – II: is the Cape Verde mid-plate swell supported by a lithosphere of varying mechanical strength?.

Rapid rates of growth and collapse of Monowai submarine volcano in the Kermadec Arc. (2012)
Journal Article
Watts, A., Peirce, C., Grevemeyer, I., Paulatto, M., Stratford, W., Bassett, D., …de Ronde, C. (2012). Rapid rates of growth and collapse of Monowai submarine volcano in the Kermadec Arc. Nature Geoscience, 5(7), 510-515. https://doi.org/10.1038/ngeo1473

Most of Earth’s volcanoes are under water. As a result of their relative inaccessibility, little is known of the structure and evolution of submarine volcanoes. Advances in navigation and sonar imaging techniques have made it possible to map submarin... Read More about Rapid rates of growth and collapse of Monowai submarine volcano in the Kermadec Arc..

Deep seismic structure of the Tonga subduction zone: Implications for mantle hydration, tectonic erosion, and arc magmatism. (2011)
Journal Article
Contreras-Reyes, E., Grevemeyer, I., Watts, A., Flueh, E., Moeller, S., Papenberg, C., & Peirce, C. (2011). Deep seismic structure of the Tonga subduction zone: Implications for mantle hydration, tectonic erosion, and arc magmatism. Journal of Geophysical Research, 116(B10), Article B10103. https://doi.org/10.1029/2011jb008434

[1] We present the first detailed 2D seismic tomographic image of the trench-outer rise, fore- and back-arc of the Tonga subduction zone. The study area is located approximately 100 km north of the collision between the Louisville hot spot track and... Read More about Deep seismic structure of the Tonga subduction zone: Implications for mantle hydration, tectonic erosion, and arc magmatism..

Contrasts in morphology and deformation offshore Montserrat: New insights from the SEA-CALIPSO marine cruise data (2010)
Journal Article
Kenedi, C., Sparks, R., Malin, P., Voight, B., Dean, S., Minshull, T., …Shalev, E. (2010). Contrasts in morphology and deformation offshore Montserrat: New insights from the SEA-CALIPSO marine cruise data. Geophysical Research Letters, 37(19), Article L00E25. https://doi.org/10.1029/2010gl043925

During the December 2007, SEA-CALIPSO experiment we collected seismic reflection profiles offshore of Montserrat. Off the east coast, we imaged deep fans of volcaniclastic debris from three volcanoes progressively active from ∼2 Ma to present. Near-s... Read More about Contrasts in morphology and deformation offshore Montserrat: New insights from the SEA-CALIPSO marine cruise data.

Seismic structure, gravity anomalies, and flexure of the Amazon continental margin, NE Brazil. (2009)
Journal Article
Watts, A., Rodger, M., Greenroyd, C., Peirce, C., & Hobbs, R. (2009). Seismic structure, gravity anomalies, and flexure of the Amazon continental margin, NE Brazil. Journal of Geophysical Research, 114(B7), Article B07103. https://doi.org/10.1029/2008jb006259

[1] Seismic and gravity data have been used to determine the structure of the sediments, crust, and upper mantle that underlie the Amazon continental margin, offshore NE Brazil. Seismic reflection profile data reveal a major unconformity at ∼7 s two-... Read More about Seismic structure, gravity anomalies, and flexure of the Amazon continental margin, NE Brazil..

Seismic constraints on the structure of the Cape Verdes swell. (2008)
Presentation / Conference Contribution
Wilson, D., Peirce, C., Watts, A., & Grevemeyer, I. (2008, December). Seismic constraints on the structure of the Cape Verdes swell. Paper presented at British Geophysical Aassociation: Postgraduates in Geophysics Meeting 2008, Durham University, UK

Crustal structure of the French Guiana margin, West Equatorial Atlantic (2007)
Journal Article
Greenroyd, C., Peirce, C., Rodger, M., Watts, A., & Hobbs, R. (2007). Crustal structure of the French Guiana margin, West Equatorial Atlantic. Geophysical Journal International, 169(3), 964-987. https://doi.org/10.1111/j.1365-246x.2007.03372.x

Geophysical data from the Amazon Cone Experiment are used to determine the structure and evolution of the French Guiana and Northeast Brazil continental margin, and to better understand the origin and development of along-margin segmentation. A 427-k... Read More about Crustal structure of the French Guiana margin, West Equatorial Atlantic.

Morphology and genesis of slow-spreading ridges - seabed scattering and seismic imaging within the oceanic crust (2007)
Journal Article
Peirce, C., Sinha, M., Topping, S., & Gill, C. (2007). Morphology and genesis of slow-spreading ridges - seabed scattering and seismic imaging within the oceanic crust. Geophysical Journal International, 168(1), 59-89. https://doi.org/10.1111/j.1365-246x.2006.03223.x

A grid of 32 across-axis and five axis-parallel multichannel seismic (MCS) reflection profiles were acquired at an axial volcanic ridge (AVR) segment at 57° 45'N, 32° 35'W on the slow-spreading Reykjanes Ridge, Mid-Atlantic Ridge, to determine the al... Read More about Morphology and genesis of slow-spreading ridges - seabed scattering and seismic imaging within the oceanic crust.

Evidence for unusually thin oceanic crust and strong mantle beneath the Amazon fan (2006)
Journal Article
Rodger, M., Watts, A., Greenroyd, C., Peirce, C., & Hobbs, R. (2006). Evidence for unusually thin oceanic crust and strong mantle beneath the Amazon fan. Geology, 34(12), 1081-1084. https://doi.org/10.1130/g22966a.1

We used seismic and gravity data to determine the structure of the crust and mantle beneath the Amazon Fan. Seismic data suggest that the crust is of oceanic-type and is unusually thin (

Temporal and spatial cyclicity of accretion at slow-spreading ridges - evidence from the Reykjanes Ridge (2005)
Journal Article
Peirce, C., Gardiner, A., & Sinha, M. (2005). Temporal and spatial cyclicity of accretion at slow-spreading ridges - evidence from the Reykjanes Ridge. Geophysical Journal International, 163(1), 56-78. https://doi.org/10.1111/j.1365-246x.2005.02738.x

A unifying model of oceanic crustal development at slow spreading rates is presented in which accretion follows a cyclic pattern of magmatic construction and tectonic destruction, controlled by along-axis variation in melt supply and coupled to along... Read More about Temporal and spatial cyclicity of accretion at slow-spreading ridges - evidence from the Reykjanes Ridge.

B-DEOS Plans for establishment of long-term mobile interdisciplinary ocean observatory systems in the N and S Atlantic, Long-term observations in the oceans, current status and perspectives for the future. (2001)
Presentation / Conference Contribution
Schultz, A., Lampitt, R., Peirce, C., & Boyle, E. (2001). B-DEOS Plans for establishment of long-term mobile interdisciplinary ocean observatory systems in the N and S Atlantic, Long-term observations in the oceans, current status and perspectives for the future.

Three-dimensional crustal structure and magma chamber geometry at the intermediate-spreading, back-arc Valu Fa Ridge, Lau Basin- results of a wide-angle seismic tomographic inversion. (2001)
Journal Article
Day, A., Peirce, C., & Sinha, M. (2001). Three-dimensional crustal structure and magma chamber geometry at the intermediate-spreading, back-arc Valu Fa Ridge, Lau Basin- results of a wide-angle seismic tomographic inversion. Geophysical Journal International, 146(1), 31-52. https://doi.org/10.1046/j.0956-540x.2001.01446.x

Magnetic survey of the Holy Island Dyke on Holy Island, Northumberland (2000)
Journal Article
Goulty, N., Peirce, C., Flatman, T., Home, M., & Richardson, J. (2000). Magnetic survey of the Holy Island Dyke on Holy Island, Northumberland. Proceedings of the Yorkshire Geological Society, 53(2), 111-118. https://doi.org/10.1144/pygs.53.2.111

The Holy Island Dyke on Holy Island, Northumberland strikes E-W along the south coast of the island. It intrudes Lower Carboniferous rocks and crops out as five discrete segments of dolerite. Flat tops on the two largest segments, benches on the sout... Read More about Magnetic survey of the Holy Island Dyke on Holy Island, Northumberland.

Bathymetry of the Reykjanes Ridge. (1997)
Journal Article
Keeton, J., Searle, R., Parsons, B., White, R., Murton, B., Parson, L., …Sinha, M. (1997). Bathymetry of the Reykjanes Ridge. Marine Geophysical Research, 19(1), 55-64

Evidence for accumulated melt beneath the slow-spreading Mid-Atlantic Ridge. In: Mid-ocean ridges - dynamics of processes associated with creation of new oceanic crust. (1997)
Journal Article
Sinha, M., Navin, D., MacGregor, L., Constable, S., Peirce, C., White, A., …Inglis, M. (1997). Evidence for accumulated melt beneath the slow-spreading Mid-Atlantic Ridge. In: Mid-ocean ridges - dynamics of processes associated with creation of new oceanic crust. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 355(1723), 233-253

Crustal structure of the Madeira-Tore Rise, eastern North Atlantic - results of a DOBS wide-angle and normal incidence seismic experiment in the Josephine Seamount region. (1991)
Journal Article
Peirce, C., & Barton, P. (1991). Crustal structure of the Madeira-Tore Rise, eastern North Atlantic - results of a DOBS wide-angle and normal incidence seismic experiment in the Josephine Seamount region. Geophysical Journal International, 106, 357-378. https://doi.org/10.1111/j.1365-246x.1991.tb03898.x