Search

Your search keyword '"Moore, Jo"' showing total 634 results
Start Over Author "Moore, Jo"

Refine your results

more »

more »

more »

more »

more »
634 results on '"Moore, Jo"'

5. Extreme hydrothermal conditions at an active plate-bounding fault

Author

Sutherland, Rupert, Townend, John, Toy, Virginia, Upton, Phaedra, Coussens, Jamie, Allen, Michael, Baratin, Laura-May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin, Boles, Austin, Boulton, Carolyn, Broderick, Neil GR, Janku-Capova, Lucie, Carpenter, Brett M, Célérier, Bernard, Chamberlain, Calum, Cooper, Alan, Coutts, Ashley, Cox, Simon, Craw, Lisa, Doan, Mai-Linh, Eccles, Jennifer, Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Howarth, Jamie, Jacobs, Katrina, Jeppson, Tamara, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Timothy, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Massiot, Cécile, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luiz, Morgan, Chance, Mori, Hiroshi, Niemeijer, Andre, Nishikawa, Osamu, Prior, David, Sauer, Katrina, Savage, Martha, Schleicher, Anja, Schmitt, Douglas R, Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, Williams, Jack, Woodman, Nick, and Zimmer, Martin

Subjects
Earth Sciences, Geophysics, General Science & Technology
Abstract

Temperature and fluid pressure conditions control rock deformation and mineralization on geological faults, and hence the distribution of earthquakes. Typical intraplate continental crust has hydrostatic fluid pressure and a near-surface thermal gradient of 31 ± 15 degrees Celsius per kilometre. At temperatures above 300-450 degrees Celsius, usually found at depths greater than 10-15 kilometres, the intra-crystalline plasticity of quartz and feldspar relieves stress by aseismic creep and earthquakes are infrequent. Hydrothermal conditions control the stability of mineral phases and hence frictional-mechanical processes associated with earthquake rupture cycles, but there are few temperature and fluid pressure data from active plate-bounding faults. Here we report results from a borehole drilled into the upper part of the Alpine Fault, which is late in its cycle of stress accumulation and expected to rupture in a magnitude 8 earthquake in the coming decades. The borehole (depth 893 metres) revealed a pore fluid pressure gradient exceeding 9 ± 1 per cent above hydrostatic levels and an average geothermal gradient of 125 ± 55 degrees Celsius per kilometre within the hanging wall of the fault. These extreme hydrothermal conditions result from rapid fault movement, which transports rock and heat from depth, and topographically driven fluid movement that concentrates heat into valleys. Shear heating may occur within the fault but is not required to explain our observations. Our data and models show that highly anomalous fluid pressure and temperature gradients in the upper part of the seismogenic zone can be created by positive feedbacks between processes of fault slip, rock fracturing and alteration, and landscape development at plate-bounding faults.

Published
2017

6. Tracking Ovine Pulmonary Adenocarcinoma Development Using an Experimental Jaagsiekte Sheep Retrovirus Infection Model.

Author

Cousens, Chris, Meehan, James, Collie, David, Wright, Steven, Chang, Ziyuan, Todd, Helen, Moore, Jo, Grant, Lynn, Daniel, Carola R., Tennant, Peter, Ritchie, Adrian, Nixon, James, Proudfoot, Chris, Guido, Stefano, Brown, Helen, Gray, Calum D., MacGillivray, Tom J., Clutton, R. Eddie, Greenhalgh, Stephen N., and Gregson, Rachael

Subjects
RETROVIRUS diseases, COMPUTED tomography, AUTOPSY, SHEEP diseases, SYSTEMS availability
Abstract

Ovine pulmonary adenocarcinoma (OPA) is an infectious, neoplastic lung disease of sheep that causes significant animal welfare and economic issues throughout the world. Understanding OPA pathogenesis is key to developing tools to control its impact. Central to this need is the availability of model systems that can monitor and track events after Jaagsiekte sheep retrovirus (JSRV) infection. Here, we report the development of an experimentally induced OPA model intended for this purpose. Using three different viral dose groups (low, intermediate and high), localised OPA tumour development was induced by bronchoscopic JSRV instillation into the segmental bronchus of the right cardiac lung lobe. Pre-clinical OPA diagnosis and tumour progression were monitored by monthly computed tomography (CT) imaging and trans-thoracic ultrasound scanning. Post mortem examination and immunohistochemistry confirmed OPA development in 89% of the JSRV-instilled animals. All three viral doses produced a range of OPA lesion types, including microscopic disease and gross tumours; however, larger lesions were more frequently identified in the low and intermediate viral groups. Overall, 31% of JSRV-infected sheep developed localised advanced lesions. Of the sheep that developed localised advanced lesions, tumour volume doubling times (calculated using thoracic CT 3D reconstructions) were 14.8 ± 2.1 days. The ability of ultrasound to track tumour development was compared against CT; the results indicated a strong significant association between paired CT and ultrasound measurements at each time point (R2 = 0.799, p < 0.0001). We believe that the range of OPA lesion types induced by this model replicates aspects of naturally occurring disease and will improve OPA research by providing novel insights into JSRV infectivity and OPA disease progression. [ABSTRACT FROM AUTHOR]

Published
2024
Full Text
View/download PDF

9. A Conceptual Framework for Research in IS/IT Instruction.

Author

Moore, Jo Ellen and Burke, Lisa A.

Abstract

This paper describes a framework for research in Information Systems/Information Technology (IS/IT) instruction that is grounded in existing theory and research from education literature. A recently developed model that integrates instructional design and learning motivation theories provides a theoretical basis for future efforts of researchers and practitioners in IS/IT instruction. Primary theories of instructional design and learning motivation are reviewed; a detailed description of the integrative model is provided, focusing on instructional methods, learner motivation, instructional conditions, and outcomes. Finally, implications for research and practice in IS/IT instruction are drawn from the integrative model. (AEF)

Published
1997

18. Melt mixing and transport across the Whale Head Rock contact aureole of the Albany-Fraser Orogen, Western Australia

Author

Moore, Jo, Gillespie, Jack, Evans, Katy, and Baumgartner, Lukas P.

Abstract

The processes that facilitate the production of granitoids are elucidated by the study of exposed lower crustal sections. The focus of this study is an exposure of the lower crustal portion of Albany-Fraser-Orogen (AFO) of Western Australia. This outcrop, located at Whale Head Rock in the western AFO, preserves the interface between an intrusive body and migmatised sedimentary rocks. Detailed mapping, petrography and thermodynamic modelling are combined to characterize the sources and distribution of melt generations in the aureole. U-Pb dating of zircon indicates that the tonalite crystallisation and migmatization of the metapelitic units were coeval at ca. 1.3 Ga. While thermodynamic modelling yields conditions of ca. 820°C and 0.5 GPa, in metapelites throughout the area. The contact zone evolves from igneous dominated textures to migmatitic sediments, dominated by concordant, internally derived leucosomes. The distribution of mineral assemblages and mineral chemistry across this section indicates that the mixing between intrusive and internally generated melt is structurally constrained. The back reaction with late stage, more evolved, melts within this mixing zone indicates that it acts as a pathway for continued melt removal and transport. This study represents and outcrop scale model for the complex processes that are involved in the production of granitoids at high temperature, medium pressure conditions. Giving further insight into the generation and extrapolation of melt from thinned crustal settings.

Published
2022
Full Text
View/download PDF

24. Microstructurally controlled trace element (Zr, U–Pb) concentrations in metamorphic rutile: An example from the amphibolites of the Bergen Arcs

Author

Moore, Jo, Beinlich, Andreas, Porter, Jennifer K., Talavera Rodriguez, Cristina, Berndt, J., Piazolo, S., Austrheim, H., Putnis, Andrew, Moore, Jo, Beinlich, Andreas, Porter, Jennifer K., Talavera Rodriguez, Cristina, Berndt, J., Piazolo, S., Austrheim, H., and Putnis, Andrew

Abstract

As a common constituent of metamorphic assemblages, rutile provides constraints on the timing and conditions of rock transformation at high resolution. However, very little is known about the links between trace element mobility and rutile microstructures that result from synmetamorphic deformation. To address this issue, here we combine in situ LA-ICP-MS and sensitive high-resolution ion microprobe trace element data with electron back-scatter diffraction microstructural analyses to investigate the links between rutile lattice distortions and Zr and U–Pb systematics. Furthermore, we apply this integrated approach to constrain further the temperature and timing of amphibolite facies metamorphism and deformation in the Bergen Arcs of southwestern Norway. In outcrop, the formation of porphyroblastic rutile in dynamically hydrated leucocratic domains of otherwise rutile-poor statically hydrated amphibolite provides key contextual information on both the ambient conditions of hydration and deformation and the composition of the reactive fluid. Rutile in amphibolite recorded ambient metamorphic temperatures of ~590–730°C during static hydration of the granulitic precursor. By contrast, rutile from leucocratic domains in the directly adjacent shear zone indicates that deformation was accompanied by a localized increase in temperature. These higher temperatures are recorded in strain-free rutile (~600–860°C) and by Zr concentration measurements on low-angle boundaries and shear bands (620–820°C). In addition, we also observe slight depletions of Zr and U along rutile low-angle boundaries relative to strain-free areas in deformed grains from the shear zone. This indicates that crystal–plastic deformation facilitated the compositional re-equilibration of rutile upon cooling to slightly below the peak temperature of deformation. Cessation of deformation at mid-crustal conditions near ~600°C is recorded by late stage growth of small (<150 µm) rutile in the high-strain zones. U

Published
2020

25. Metamorphic differentiation via enhanced dissolution along high permeability zones

Author

Moore, Jo, Beinlich, Andreas, Piazolo, S., Austrheim, H., Putnis, Andrew, Moore, Jo, Beinlich, Andreas, Piazolo, S., Austrheim, H., and Putnis, Andrew

Abstract

Metamorphic differentiation, resulting in segregated mineral bands, is commonly recorded in metamorphic rocks. Despite the ubiquitous nature of compositionally layered metamorphic rocks, the processes that are responsible for metamorphic differentiation receive very little attention. Here, detailed petrography, quantitative mineral chemistry and bulk rock analyses are applied to investigate compositional variations and assemblage microstructure. Furthermore, thermodynamic modelling is applied to provide additional constraints on the P-T-XH2O conditions of assemblage formation and mass transfer. The studied outcrop, located within the Bergen arcs of southwestern Norway, preserves the hydration of anorthositic granulite at amphibolite-facies conditions. The amphibolite-facies hydration is expressed as both a statically hydrated amphibolite and a shear zone lithology, defined by the interlayering of amphibolite with leucocratic domains. Within the granulite, quartz-lined fractures surrounded by amphibolite-facies alteration haloes represent relics of initial fluid infiltration associated with brittle failure. The fracture assemblage (quartz + plagioclase + zoisite + kyanite ± muscovite ± biotite) is identical to that occurring within leucocratic domains of the shear zone. Consequently, the compositional layering of the shear zone lithology is linked to fluid infiltration along localized zones of high permeability that result from fracturing. Mass-balance calculations indicate that quartz-lined fractures and compositional differentiation of the shear zone resulted from mass redistribution internal to the shear zone rather than partial melting or precipitation of minerals from externally derived fluid. The process of internal fractionation within the shear zone is driven by enhanced dissolution along highly permeable fracture planes resulting in the loss of MgO, Fetot and K2O from the leucocratic domains. Elements dissolved in the fluid are then transported and ultimatel

Published
2020

29. Vortex velocity laws to I-V data for flat superconductors

Author

Jonathan Chapman, S., Grief, Andrew D., Howison, Sam D., McCulloch, Malcolm D., Dew-Huges, David, Moore, Jo, and Grovenor, Chris M.

Subjects
Superconductors -- Research, Business, Electronics, Electronics and electrical industries
Abstract

Transport current in flux-flow conditions was studied using a vortex-density model for type-II superconductors.

Published
2001

37. Synthesis and properties of thallium based superconducting wire and tape

Author

Wivell, Simon K., Fox, Simon, Moore, Jo C., and Grovenor, Chris R.M.

Subjects
High temperature superconductors, Thallium compounds, Business, Electronics, Electronics and electrical industries
Abstract

The preparation of superconducting wires and tapes from the (Tl.05Pb0.5)(Sr1.6Ba0.4)Ca2Cu3Ox and (Tl0.78Bi0.22)(Sr1.6Ba0.4)Ca2Cu3Ox phases using lead or bismuth dopants and pure silver or silver alloy tubes were investigated. Specifically, the drawing and rolling processes required to achieve the best core uniformity are examined along with the heat treatment that produces the highest critical current density values.

Published
1995

39. The focus of research in end user computing: where have we come since the 1980s?

Author

Powell, Anne and Moore, Jo Ellen

Subjects
User need, Company business management, End user, End users, End-user computing -- Management
Abstract

During the 1980s, end user computing was often the domain of early adopters or 'techies.' But during the 1990s, the information technology (IT) revolution reached almost everyone in business organizations. […]

Published
2002

42. Contemporary satire of corporate managers: time to cut the boss some slack

Author

Burke, Lisa A. and Moore, Jo Ellen

Subjects
Dilbert (Comic strip) -- Criticism and interpretation, Executives -- Portrayals -- Analysis -- Methods, Management -- Methods -- Analysis, Satire -- Analysis -- Methods, Business, general, Business, Criticism and interpretation, Analysis, Portrayals, Methods
Abstract

We have all read the cartoons that poke fun at corporate managers, and have broken into smiles or laughter at their intended humor. Developed and reinforced by the popular media, [...]

Published
1999

43. Are you burning out valuable resources?

Author

Moore, Jo Ellen

Subjects
Job stress -- Management, Burn out (Psychology) -- Management, Employee morale -- Analysis, Human resource management ) -- Methods, Work environment -- Management, Business, Human resources and labor relations
Abstract

Burn out is one of the reasons behind high employee turnovers in high technology industries and other markets. The common victims of burn out are the highly motivated and committed employees. Thus, human resource professionals must coordinate with department heads to effectively manage this occupational malady. Identifying the exact cause of exhaustion and analyzing the work set-up must be foremost in eliminating or minimizing the problem. Prescribing processes and practices that control job stress can protect employees from burn out and from possibly leaving their jobs., Top performing, motivated workers are the ones most susceptible to burnout. Retaining valued workers, particularly technology workers, has become crucial for many organizations in today's tight labor market. At the [...]

Published
1999

44. Studies of the transmissibility of the agent of bovine spongiform encephalopathy to the domestic chicken

Author

Moore Jo, Hawkins Stephen AC, Austin Anthony R, Konold Timm, Green Robert B, Blamire Ian W, Dexter Ian, Stack Michael J, Chaplin Melanie J, Langeveld Jan PM, Simmons Marion M, Spencer Yvonne I, Webb Paul R, Dawson Michael, and Wells Gerald AH

Subjects
Medicine, Biology (General), QH301-705.5, Science (General), Q1-390
Abstract

Abstract Background Transmission of the prion disease bovine spongiform encephalopathy (BSE) occurred accidentally to cattle and several other mammalian species via feed supplemented with meat and bone meal contaminated with infected bovine tissue. Prior to United Kingdom controls in 1996 on the feeding of mammalian meat and bone meal to farmed animals, the domestic chicken was potentially exposed to feed contaminated with the causal agent of BSE. Although confirmed prion diseases are unrecorded in avian species a study was undertaken to transmit BSE to the domestic chicken by parenteral and oral inoculations. Transmissibility was assessed by clinical monitoring, histopathological examinations, detection of a putative disease form of an avian prion protein (PrP) in recipient tissues and by mouse bioassay of tissues. Occurrence of a progressive neurological syndrome in the primary transmission study was investigated by sub-passage experiments. Results No clinical, pathological or bioassay evidence of transmission of BSE to the chicken was obtained in the primary or sub-passage experiments. Survival data showed no significant differences between control and treatment groups. Neurological signs observed, not previously described in the domestic chicken, were not associated with significant pathology. The diagnostic techniques applied failed to detect a disease associated form of PrP. Conclusion Important from a risk assessment perspective, the present study has established that the domestic chicken does not develop a prion disease after large parenteral exposures to the BSE agent or after oral exposures equivalent to previous exposures via commercial diets. Future investigations into the potential susceptibility of avian species to mammalian prion diseases require species-specific immunochemical techniques and more refined experimental models.

Published
2011
Full Text
View/download PDF

48. Petrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture-Mediated Fluid and Heat Transport in the Alpine Fault's Hanging-Wall Damage Zone

Author

Townend, John, Sutherland, Rupert, Toy, Virginia G., Doan, Mai Linh, Célérier, Bernard, Massiot, Cécile, Coussens, Jamie, Jeppson, Tamara, Janku-Capova, Lucie, Remaud, Léa, Upton, Phaedra, Schmitt, Douglas R., Pezard, Philippe, Williams, Jack, Allen, Michael John, Baratin, Laura May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin M., Boulton, Carolyn, Broderick, Neil G.R., Carpenter, Brett M., Chamberlain, Calum J., Cooper, Alan, Coutts, Ashley, Cox, Simon C., Craw, Lisa, Eccles, Jennifer D., Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Henry, Gilles, Howarth, Jamie, Jacobs, Katrina, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Tim, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luis, Mori, Hiroshi, Niemeijer, André, Nishikawa, Osamu, Nitsch, Olivier, Paris, Jehanne, Prior, David J., Sauer, Katrina, Savage, Martha K., Schleicher, Anja, Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon A H, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, Zimmer, Martin, Townend, John, Sutherland, Rupert, Toy, Virginia G., Doan, Mai Linh, Célérier, Bernard, Massiot, Cécile, Coussens, Jamie, Jeppson, Tamara, Janku-Capova, Lucie, Remaud, Léa, Upton, Phaedra, Schmitt, Douglas R., Pezard, Philippe, Williams, Jack, Allen, Michael John, Baratin, Laura May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin M., Boulton, Carolyn, Broderick, Neil G.R., Carpenter, Brett M., Chamberlain, Calum J., Cooper, Alan, Coutts, Ashley, Cox, Simon C., Craw, Lisa, Eccles, Jennifer D., Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Henry, Gilles, Howarth, Jamie, Jacobs, Katrina, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Tim, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luis, Mori, Hiroshi, Niemeijer, André, Nishikawa, Osamu, Nitsch, Olivier, Paris, Jehanne, Prior, David J., Sauer, Katrina, Savage, Martha K., Schleicher, Anja, Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon A H, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, and Zimmer, Martin

Abstract

Fault rock assemblages reflect interaction between deformation, stress, temperature, fluid, and chemical regimes on distinct spatial and temporal scales at various positions in the crust. Here we interpret measurements made in the hanging-wall of the Alpine Fault during the second stage of the Deep Fault Drilling Project (DFDP-2). We present observational evidence for extensive fracturing and high hanging-wall hydraulic conductivity (∼10-9 to 10-7 m/s, corresponding to permeability of ∼10-16 to 10-14 m2) extending several hundred meters from the fault's principal slip zone. Mud losses, gas chemistry anomalies, and petrophysical data indicate that a subset of fractures intersected by the borehole are capable of transmitting fluid volumes of several cubic meters on time scales of hours. DFDP-2 observations and other data suggest that this hydrogeologically active portion of the fault zone in the hanging-wall is several kilometers wide in the uppermost crust. This finding is consistent with numerical models of earthquake rupture and off-fault damage. We conclude that the mechanically and hydrogeologically active part of the Alpine Fault is a more dynamic and extensive feature than commonly described in models based on exhumed faults. We propose that the hydrogeologically active damage zone of the Alpine Fault and other large active faults in areas of high topographic relief can be subdivided into an inner zone in which damage is controlled principally by earthquake rupture processes and an outer zone in which damage reflects coseismic shaking, strain accumulation and release on interseismic timescales, and inherited fracturing related to exhumation.

Published
2017

49. Extreme hydrothermal conditions at an active plate-bounding fault

Author

Experimental rock deformation, Sutherland, Rupert, Townend, John, Toy, Virginia, Upton, Phaedra, Coussens, Jamie, Allen, Michael, Baratin, Laura May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin, Boles, Austin, Boulton, Carolyn, Broderick, Neil G.R., Janku-Capova, Lucie, Carpenter, Brett M., Célérier, Bernard, Chamberlain, Calum, Cooper, Alan, Coutts, Ashley, Cox, Simon, Craw, Lisa, Doan, Mai Linh, Eccles, Jennifer, Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Howarth, Jamie, Jacobs, Katrina, Jeppson, Tamara, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Timothy, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Massiot, Cécile, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luiz, Morgan, Chance, Mori, Hiroshi, Niemeijer, Andre, Nishikawa, Osamu, Prior, David, Sauer, Katrina, Savage, Martha, Schleicher, Anja, Schmitt, Douglas R., Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, Williams, Jack, Woodman, Nick, Zimmer, Martin, Experimental rock deformation, Sutherland, Rupert, Townend, John, Toy, Virginia, Upton, Phaedra, Coussens, Jamie, Allen, Michael, Baratin, Laura May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin, Boles, Austin, Boulton, Carolyn, Broderick, Neil G.R., Janku-Capova, Lucie, Carpenter, Brett M., Célérier, Bernard, Chamberlain, Calum, Cooper, Alan, Coutts, Ashley, Cox, Simon, Craw, Lisa, Doan, Mai Linh, Eccles, Jennifer, Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Howarth, Jamie, Jacobs, Katrina, Jeppson, Tamara, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Timothy, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Massiot, Cécile, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luiz, Morgan, Chance, Mori, Hiroshi, Niemeijer, Andre, Nishikawa, Osamu, Prior, David, Sauer, Katrina, Savage, Martha, Schleicher, Anja, Schmitt, Douglas R., Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, Williams, Jack, Woodman, Nick, and Zimmer, Martin

Published
2017

50. Petrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture-Mediated Fluid and Heat Transport in the Alpine Fault's Hanging-Wall Damage Zone

Author

Experimental rock deformation, Townend, John, Sutherland, Rupert, Toy, Virginia G., Doan, Mai Linh, Célérier, Bernard, Massiot, Cécile, Coussens, Jamie, Jeppson, Tamara, Janku-Capova, Lucie, Remaud, Léa, Upton, Phaedra, Schmitt, Douglas R., Pezard, Philippe, Williams, Jack, Allen, Michael John, Baratin, Laura May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin M., Boulton, Carolyn, Broderick, Neil G.R., Carpenter, Brett M., Chamberlain, Calum J., Cooper, Alan, Coutts, Ashley, Cox, Simon C., Craw, Lisa, Eccles, Jennifer D., Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Henry, Gilles, Howarth, Jamie, Jacobs, Katrina, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Tim, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luis, Mori, Hiroshi, Niemeijer, André, Nishikawa, Osamu, Nitsch, Olivier, Paris, Jehanne, Prior, David J., Sauer, Katrina, Savage, Martha K., Schleicher, Anja, Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon A H, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, Zimmer, Martin, Experimental rock deformation, Townend, John, Sutherland, Rupert, Toy, Virginia G., Doan, Mai Linh, Célérier, Bernard, Massiot, Cécile, Coussens, Jamie, Jeppson, Tamara, Janku-Capova, Lucie, Remaud, Léa, Upton, Phaedra, Schmitt, Douglas R., Pezard, Philippe, Williams, Jack, Allen, Michael John, Baratin, Laura May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin M., Boulton, Carolyn, Broderick, Neil G.R., Carpenter, Brett M., Chamberlain, Calum J., Cooper, Alan, Coutts, Ashley, Cox, Simon C., Craw, Lisa, Eccles, Jennifer D., Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Henry, Gilles, Howarth, Jamie, Jacobs, Katrina, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Tim, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luis, Mori, Hiroshi, Niemeijer, André, Nishikawa, Osamu, Nitsch, Olivier, Paris, Jehanne, Prior, David J., Sauer, Katrina, Savage, Martha K., Schleicher, Anja, Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon A H, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, and Zimmer, Martin

Published
2017

Catalog

Books, media, physical & digital resources
See catalog results