no. 2531.

Funck, T., Jackson, H. R., Louden, K. E., Dehler, S. A., and Wu, Y. (2004). Crustal structure of the northern Nova Scotia rifted continental margin (eastern Canada). *J. Geophys. Res.: Solid Earth*, 109(B9), article no. B09102.

Gautier, P., Brun, J. P., and Jolivet, L. (1993). Structure and kinematics of upper Cenozoic extensional detachment on Naxos and Paros (Cyclades Islands, Greece). *Tectonics*, 12(5), 1180–1194.

Geoffroy, L., Burov, E., and Werner, P. (2015). Volcanic passive margins: another way to break up continents. *Sci. Rep.*, 5, article no. 14828.

Gerya, T. V. and Yuen, D. A. (2003). Characteristics-based marker-in-cell method with conservative finite-differences schemes for modeling geological flows with strongly variable transport properties. *Phys. Earth Planet. Inter.*, 140(4), 293–318.

Gillard, M., Tugend, J., Müntener, O., Manatschal, G., Karner, G. D., Autin, J., et al. (2019). The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins. *Earth-Sci. Rev.*, 196, article no. 102882.

Goetze, C. and Evans, B. (1979). Stress and temperature in the bending lithosphere as constrained by experimental rock mechanics. *Geophys. J. Int.*, 59(3), 463–478.

Gomez-Romeu, J., Kusznir, N., Roberts, A., and Manatschal, G. (2020). Measurements of the extension required for crustal breakup on the magma-poor Iberia-Newfoundland conjugate margins. *Mar. Petrol. Geol.*, 118, article no. 104403.

Gresseth, J. L. S., Osmundsen, P. T., and Péron-Pinvidic, G. (2023). 3D evolution of detachment fault systems in necking domains: Insights from the Klakk Fault Complex and the Froya High, mid-Norwegian rifted margin. *Tectonics*, 42(3), article no. e2022TC007600.

Gueydan, F., Leroy, Y. M., and Jolivet, L. (2001). Grain-size-sensitive flow and shear-stress enhancement at the brittle–ductile transition of the continental crust. *Int. J. Earth Sci.*, 90(1), 181–196.

Gueydan, F., Morency, C., and Brun, J. P. (2008). Continental rifting as a function of lithosphere mantle strength. *Tectonophysics*, 460(1–4), 83–93.

Gueydan, F., Pitra, P., Afiri, A., Poujol, M., Essaifi, A., and Paquette, J. L. (2015). Oligo-Miocene thinning of the Beni Bousera peridotites and their Variscan crustal host rocks, Internal Rif, Morocco. *Tectonics*,

34(6), 1244–1268.

Handy, M. R. and Zingg, A. (1991). The tectonic and rheological evolution of an attenuated cross section of the continental crust: Ivrea crustal section, southern Alps, northwestern Italy and southern Switzerland. *Geol. Soc. Am. Bull.*, 103(2), 236–253.

Hansen, F. D. and Carter, N. L. (1983). Semibrittle creep of dry and wet Westerly Granite at 1000 MPa. In *The 24th U.S. Symposium on Rock Mechanics (USRMS), College Station, Texas, June 20*. ARMA-83-0429.

Heezen, B. C. (1960). The rift in the ocean floor. *Sci. Am.*, 203(4), 98–114.

Hirth, G. and Kohlstedt, D. (2004). Rheology of the upper mantle and the mantle wedge: A view from the experimentalists. In *Inside the Subduction Factory*, pages 83–105. American Geophysical Union (AGU), Washington, DC.

Hölker, A. B., Manatschal, G., Holliger, K., and Bernoulli, D. (2003). Tectonic nature and seismic response of top-basement detachment faults in magma-poor rifted margins. *Tectonics*, 22(4), article no. 1035.

Hopper, J. R. and Buck, W. R. (1996). The effect of lower crustal flow on continental extension and passive margin formation. *J. Geophys. Res.: Solid Earth*, 101(B9), 20175–20194.

Huet, B., Le Pourhiet, L., Labrousse, L., Burov, E., and Jolivet, L. (2011a). Post-orogenic extension and metamorphic core complexes in a heterogeneous crust: the role of crustal layering inherited from collision. Application to the Cyclades ( Aegean domain). *Geophys. J. Int.*, 184(2), 611–625.

Huet, B., Le Pourhiet, L., Labrousse, L., Burov, E. B., and Jolivet, L. (2011b). Formation of metamorphic core complex in inherited wedges: A thermomechanical modelling study. *Earth Planet. Sci. Lett.*, 309(3–4), 249–257.

Huismans, R. and Beaumont, C. (2011). Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins. *Nature*, 473(7345), 74–78.

Huismans, R. S. and Beaumont, C. (2003). Symmetric and asymmetric lithospheric extension: Relative effects of frictional-plastic and viscous strain softening. *J. Geophys. Res.: Solid Earth*, 108(B10), article no. 2496.

Huismans, R. S. and Beaumont, C. (2007). Roles of
no. 2531.

Funck, T., Jackson, H. R., Louden, K. E., Dehler, S. A., and Wu, Y. (2004). Crustal structure of the northern Nova Scotia rifted continental margin (eastern Canada). *J. Geophys. Res.: Solid Earth*, 109(B9), article no. B09102.

Gautier, P., Brun, J. P., and Jolivet, L. (1993). Structure and kinematics of upper Cenozoic extensional detachment on Naxos and Paros (Cyclades Islands, Greece). *Tectonics*, 12(5), 1180–1194.

Geoffroy, L., Burov, E., and Werner, P. (2015). Volcanic passive margins: another way to break up continents. *Sci. Rep.*, 5, article no. 14828.

Gerya, T. V. and Yuen, D. A. (2003). Characteristics-based marker-in-cell method with conservative finite-differences schemes for modeling geological flows with strongly variable transport properties. *Phys. Earth Planet. Inter.*, 140(4), 293–318.

Gillard, M., Tugend, J., Müntener, O., Manatschal, G., Karner, G. D., Autin, J., et al. (2019). The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins. *Earth-Sci. Rev.*, 196, article no. 102882.

Goetze, C. and Evans, B. (1979). Stress and temperature in the bending lithosphere as constrained by experimental rock mechanics. *Geophys. J. Int.*, 59(3), 463–478.

Gomez-Romeu, J., Kusznir, N., Roberts, A., and Manatschal, G. (2020). Measurements of the extension required for crustal breakup on the magma-poor Iberia-Newfoundland conjugate margins. *Mar. Petrol. Geol.*, 118, article no. 104403.

Gresseth, J. L. S., Osmundsen, P. T., and Péron-Pinvidic, G. (2023). 3D evolution of detachment fault systems in necking domains: Insights from the Klakk Fault Complex and the Froya High, mid-Norwegian rifted margin. *Tectonics*, 42(3), article no. e2022TC007600.

Gueydan, F., Leroy, Y. M., and Jolivet, L. (2001). Grain-size-sensitive flow and shear-stress enhancement at the brittle–ductile transition of the continental crust. *Int. J. Earth Sci.*, 90(1), 181–196.

Gueydan, F., Morency, C., and Brun, J. P. (2008). Continental rifting as a function of lithosphere mantle strength. *Tectonophysics*, 460(1–4), 83–93.

Gueydan, F., Pitra, P., Afiri, A., Poujol, M., Essaifi, A., and Paquette, J. L. (2015). Oligo-Miocene thinning of the Beni Bousera peridotites and their Variscan crustal host rocks, Internal Rif, Morocco. *Tectonics*,

34(6), 1244–1268.

Handy, M. R. and Zingg, A. (1991). The tectonic and rheological evolution of an attenuated cross section of the continental crust: Ivrea crustal section, southern Alps, northwestern Italy and southern Switzerland. *Geol. Soc. Am. Bull.*, 103(2), 236–253.

Hansen, F. D. and Carter, N. L. (1983). Semibrittle creep of dry and wet Westerly Granite at 1000 MPa. In *The 24th U.S. Symposium on Rock Mechanics (USRMS), College Station, Texas, June 20*. ARMA-83-0429.

Heezen, B. C. (1960). The rift in the ocean floor. *Sci. Am.*, 203(4), 98–114.

Hirth, G. and Kohlstedt, D. (2004). Rheology of the upper mantle and the mantle wedge: A view from the experimentalists. In *Inside the Subduction Factory*, pages 83–105. American Geophysical Union (AGU), Washington, DC.

Hölker, A. B., Manatschal, G., Holliger, K., and Bernoulli, D. (2003). Tectonic nature and seismic response of top-basement detachment faults in magma-poor rifted margins. *Tectonics*, 22(4), article no. 1035.

Hopper, J. R. and Buck, W. R. (1996). The effect of lower crustal flow on continental extension and passive margin formation. *J. Geophys. Res.: Solid Earth*, 101(B9), 20175–20194.

Huet, B., Le Pourhiet, L., Labrousse, L., Burov, E., and Jolivet, L. (2011a). Post-orogenic extension and metamorphic core complexes in a heterogeneous crust: the role of crustal layering inherited from collision. Application to the Cyclades ( Aegean domain). *Geophys. J. Int.*, 184(2), 611–625.

Huet, B., Le Pourhiet, L., Labrousse, L., Burov, E. B., and Jolivet, L. (2011b). Formation of metamorphic core complex in inherited wedges: A thermomechanical modelling study. *Earth Planet. Sci. Lett.*, 309(3–4), 249–257.

Huismans, R. and Beaumont, C. (2011). Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins. *Nature*, 473(7345), 74–78.

Huismans, R. S. and Beaumont, C. (2003). Symmetric and asymmetric lithospheric extension: Relative effects of frictional-plastic and viscous strain softening. *J. Geophys. Res.: Solid Earth*, 108(B10), article no. 2496.

Huismans, R. S. and Beaumont, C. (2007). Roles of
lithospheric strain softening and heterogeneity in determining the geometry of rifts and continental margins. *Geol. Soc. Lond. Spec. Publ.*, 282(1), 111–138.

Huismans, R. S. and Beaumont, C. (2014). Rifted continental margins: The case for depth-dependent extension. *Earth Planet. Sci. Lett.*, 407, 148–162.

Huismans, R. S., Buiter, S. J., and Beaumont, C. (2005). Effect of plastic-viscous layering and strain softening on mode selection during lithospheric extension. *J. Geophys. Res.: Solid Earth*, 110(B2), article no. B02406.

Huismans, R. S., Podladchikov, Y. Y., and Cloetingh, S. (2001). Transition from passive to active rifting: Relative importance of asthenospheric doming and passive extension of the lithosphere. *J. Geophys. Res.: Solid Earth*, 106(B6), 11271–11291.

Jammes, S. and Lavier, L. L. (2016). The effect of bimineralic composition on extensional processes at lithospheric scale. *Geochem. Geophys. Geosyst.*, 17(8), 3375–3392.

Jammes, S., Manatschal, G., Lavier, L., and Masini, E. (2009). Tectonosedimentary evolution related to extreme crustal thinning ahead of a propagating ocean: Example of the western Pyrenees. *Tectonics*, 28(4), article no. TC4012.

Jamtveit, B., Austrheim, H., and Putnis, A. (2016). Disequilibrium metamorphism of stressed lithosphere. *Earth-Sci. Rev.*, 154, 1–13.

Jeanniot, L., Kusznir, N., Mohn, G., Manatschal, G., and Cowie, L. (2016). Constraining lithosphere deformation modes during continental breakup for the Iberia–Newfoundland conjugate rifted margins. *Tectonophysics*, 680, 28–49.

Jolivet, L., Gorini, C., Smit, J., and Leroy, S. (2015). Continental breakup and the dynamics of rifting in back-arc basins: The Gulf of Lion margin. *Tectonics*, 34(4), 662–679.

Jolivet, L., Lecomte, E., Huet, B., Denèle, Y., Lacombe, O., Labrousse, L., et al. (2010). The north Cycladic detachment system. *Earth Planet. Sci. Lett.*, 289(1–2), 87–104.

Jourdon, A., Kergaravat, C., Duclaux, G., and Huguen, C. (2021). Looking beyond kinematics: 3D thermomechanical modelling reveals the dynamic of transform margins. *Solid Earth Discuss.*, 2021, 1–34.

Jourdon, A., Le Pourhiet, L., Mouthereau, F., and May, D. (2020). Modes of propagation of continental breakup and associated oblique rift structures. *J. Geophys. Res.: Solid Earth*, 125(9), article no. e2020JB019906.

Kaczmarek, M. A. and Müntener, O. (2008). Juxtaposition of melt impregnation and high-temperature shear zones in the upper mantle; field and petrological constraints from the Lanzo Peridotite (Northern Italy). *J. Petrol.*, 49(12), 2187–2220.

Kaczmarek, M. A. and Tommasi, A. (2011). Anatomy of an extensional shear zone in the mantle, Lanzo massif, Italy. *Geochem. Geophys. Geosyst.*, 12(8), article no. Q0AG06.

Kameyama, M., Yuen, D. A., and Karato, S.-I. (1999). Thermal-mechanical effects of low-temperature plasticity (the peierls mechanism) on the deformation of a viscoelastic shear zone. *Earth Planet. Sci. Lett.*, 168(1), 159–172.

Kusznir, N. J. (1991). The distribution of stress with depth in the lithosphere: thermo-rheological and geodynamic constraints. *Philos. Trans. R. Soc. Lond. A*, 337(1645), 95–110.

Kusznir, N. J., Hunsdale, R., Roberts, A. M., and iSIMM Team (2005). Timing and magnitude of depth-dependent lithosphere stretching on the southern Lofoten and northern Vöring continental margins offshore mid-Norway: implications for subsidence and hydrocarbon maturation at volcanic rifted margins. In *Geological Society, London, Petroleum Geology Conference Series*, volume 6, pages 767–783. Geological Society of London.

Kusznir, N. J. and Karner, G. D. (2007). Continental lithospheric thinning and breakup in response to upwelling divergent mantle flow: application to the Woodlark, Newfoundland and Iberia margins. *Geol. Soc. Lond. Spec. Publ.*, 282(1), 389–419.

Kusznir, N. J., Roberts, A. M., and Morley, C. K. (1995). Forward and reverse modelling of rift basin formation. *Geol. Soc. Lond. Spec. Publ.*, 80(1), 33–56.

Lagabrielle, Y., Asti, R., Fourcade, S., Corre, B., Labaume, P., Uzel, J., et al. (2019). Mantle exhumation at magma-poor passive continental margins. Part II: Tectonic and metasomatic evolution of large-displacement detachment faults preserved in a fossil distal margin domain (Saraillé lherzolites, northwestern Pyrenees, France). *Bull. Soc. Géol. Fr.*, 190(1), article no. 14.

Lagabrielle, Y. and Bodinier, J. L. (2008). Submarine reworking of exhumed subcontinental mantle rocks: field evidence from the Lherz peridotites,
lithospheric strain softening and heterogeneity in determining the geometry of rifts and continental margins. *Geol. Soc. Lond. Spec. Publ.*, 282(1), 111–138.

Huismans, R. S. and Beaumont, C. (2014). Rifted continental margins: The case for depth-dependent extension. *Earth Planet. Sci. Lett.*, 407, 148–162.

Huismans, R. S., Buiter, S. J., and Beaumont, C. (2005). Effect of plastic-viscous layering and strain softening on mode selection during lithospheric extension. *J. Geophys. Res.: Solid Earth*, 110(B2), article no. B02406.

Huismans, R. S., Podladchikov, Y. Y., and Cloetingh, S. (2001). Transition from passive to active rifting: Relative importance of asthenospheric doming and passive extension of the lithosphere. *J. Geophys. Res.: Solid Earth*, 106(B6), 11271–11291.

Jammes, S. and Lavier, L. L. (2016). The effect of bimineralic composition on extensional processes at lithospheric scale. *Geochem. Geophys. Geosyst.*, 17(8), 3375–3392.

Jammes, S., Manatschal, G., Lavier, L., and Masini, E. (2009). Tectonosedimentary evolution related to extreme crustal thinning ahead of a propagating ocean: Example of the western Pyrenees. *Tectonics*, 28(4), article no. TC4012.

Jamtveit, B., Austrheim, H., and Putnis, A. (2016). Disequilibrium metamorphism of stressed lithosphere. *Earth-Sci. Rev.*, 154, 1–13.

Jeanniot, L., Kusznir, N., Mohn, G., Manatschal, G., and Cowie, L. (2016). Constraining lithosphere deformation modes during continental breakup for the Iberia–Newfoundland conjugate rifted margins. *Tectonophysics*, 680, 28–49.

Jolivet, L., Gorini, C., Smit, J., and Leroy, S. (2015). Continental breakup and the dynamics of rifting in back-arc basins: The Gulf of Lion margin. *Tectonics*, 34(4), 662–679.

Jolivet, L., Lecomte, E., Huet, B., Denèle, Y., Lacombe, O., Labrousse, L., et al. (2010). The north Cycladic detachment system. *Earth Planet. Sci. Lett.*, 289(1–2), 87–104.

Jourdon, A., Kergaravat, C., Duclaux, G., and Huguen, C. (2021). Looking beyond kinematics: 3D thermomechanical modelling reveals the dynamic of transform margins. *Solid Earth Discuss.*, 2021, 1–34.

Jourdon, A., Le Pourhiet, L., Mouthereau, F., and May, D. (2020). Modes of propagation of continental breakup and associated oblique rift structures. *J. Geophys. Res.: Solid Earth*, 125(9), article no. e2020JB019906.

Kaczmarek, M. A. and Müntener, O. (2008). Juxtaposition of melt impregnation and high-temperature shear zones in the upper mantle; field and petrological constraints from the Lanzo Peridotite (Northern Italy). *J. Petrol.*, 49(12), 2187–2220.

Kaczmarek, M. A. and Tommasi, A. (2011). Anatomy of an extensional shear zone in the mantle, Lanzo massif, Italy. *Geochem. Geophys. Geosyst.*, 12(8), article no. Q0AG06.

Kameyama, M., Yuen, D. A., and Karato, S.-I. (1999). Thermal-mechanical effects of low-temperature plasticity (the peierls mechanism) on the deformation of a viscoelastic shear zone. *Earth Planet. Sci. Lett.*, 168(1), 159–172.

Kusznir, N. J. (1991). The distribution of stress with depth in the lithosphere: thermo-rheological and geodynamic constraints. *Philos. Trans. R. Soc. Lond. A*, 337(1645), 95–110.

Kusznir, N. J., Hunsdale, R., Roberts, A. M., and iSIMM Team (2005). Timing and magnitude of depth-dependent lithosphere stretching on the southern Lofoten and northern Vöring continental margins offshore mid-Norway: implications for subsidence and hydrocarbon maturation at volcanic rifted margins. In *Geological Society, London, Petroleum Geology Conference Series*, volume 6, pages 767–783. Geological Society of London.

Kusznir, N. J. and Karner, G. D. (2007). Continental lithospheric thinning and breakup in response to upwelling divergent mantle flow: application to the Woodlark, Newfoundland and Iberia margins. *Geol. Soc. Lond. Spec. Publ.*, 282(1), 389–419.

Kusznir, N. J., Roberts, A. M., and Morley, C. K. (1995). Forward and reverse modelling of rift basin formation. *Geol. Soc. Lond. Spec. Publ.*, 80(1), 33–56.

Lagabrielle, Y., Asti, R., Fourcade, S., Corre, B., Labaume, P., Uzel, J., et al. (2019). Mantle exhumation at magma-poor passive continental margins. Part II: Tectonic and metasomatic evolution of large-displacement detachment faults preserved in a fossil distal margin domain (Saraillé lherzolites, northwestern Pyrenees, France). *Bull. Soc. Géol. Fr.*, 190(1), article no. 14.

Lagabrielle, Y. and Bodinier, J. L. (2008). Submarine reworking of exhumed subcontinental mantle rocks: field evidence from the Lherz peridotites,
French Pyrenees. *Terra Nova*, 20(1), 11–21.

Larsen, H. C., Mohn, G., Nirrengarten, M., Sun, Z., Stock, J., Jian, Z., et al. (2018). Rapid transition from continental breakup to igneous oceanic crust in the South China Sea. *Nat. Geosci.*, 11(10), 782–789.

Larvet, T., Le Pourhiet, L., Pubellier, M., and Gyomlai, T. (2023). Slab pull driven south China sea opening implies a Mesozoic proto South China Sea. *Geo-phys. Res. Lett.*, 50(22), article no. e2023GL105292.

Lau, K. H., Louden, K. E., Funck, T., Tucholke, B. E., Holbrook, W. S., Hopper, J. R., and Christian Larsen, H. (2006). Crustal structure across the Grand Banks—Newfoundland Basin Continental Margin—I. Results from a seismic refraction profile. *Geophys. J. Int.*, 167(1), 127–156.

Lavier, L. L. and Buck, W. R. (2002). Half graben versus large-offset low-angle normal fault: Importance of keeping cool during normal faulting. *J. Geophys. Res.: Solid Earth*, 107(B6), article no. ETG-8.

Lavier, L. L. and Manatschal, G. (2006). A mechanism to thin the continental lithosphere at magma-poor margins. *Nature*, 440(7082), 324–328.

Lavier, L. L., Roger Buck, W., and Poliakov, A. N. (1999). Self-consistent rolling-hinge model for the evolution of large-offset low-angle normal faults. *Geology*, 27(12), 1127–1130.

Le Pichon, X. and Barbier, F. (1987). Passive margin formation by low-angle faulting within the upper crust: The northern Bay of Biscay margin. *Tectonics*, 6(2), 133–150.

Le Pourhiet, L., Burov, E., and Moretti, I. (2004). Rifting through a stack of inhomogeneous thrusts (the dipping pie concept). *Tectonics*, 23(4), article no. TC4005.

Le Pourhiet, L., Chamot-Rooke, N., Delescluse, M., May, D. A., Watremez, L., and Pubellier, M. (2018). Continental break-up of the South China Sea stalled by far-field compression. *Nat. Geosci.*, 11(8), 605–609.

Le Pourhiet, L., May, D. A., Huille, L., Watremez, L., and Leroy, S. (2017). A genetic link between transform and hyper-extended margins. *Earth Planet. Sci. Lett.*, 465, 184–192.

Lecomte, E., Le Pourhiet, L., and Lacombe, O. (2012). Mechanical basis for slip along low-angle normal faults. *Geophys. Res. Lett.*, 39(3), article no. L03307.

Lecomte, E., Le Pourhiet, L., Lacombe, O., and Jolivet,

L. (2011). A continuum mechanics approach to quantify brittle strain on weak faults: application to the extensional reactivation of shallow dipping discontinuities. *Geophys. J. Int.*, 184(1), 1–11.

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Larsen, H. C., Mohn, G., Nirrengarten, M., Sun, Z., Stock, J., Jian, Z., et al. (2018). Rapid transition from continental breakup to igneous oceanic crust in the South China Sea. *Nat. Geosci.*, 11(10), 782–789.

Larvet, T., Le Pourhiet, L., Pubellier, M., and Gyomlai, T. (2023). Slab pull driven south China sea opening implies a Mesozoic proto South China Sea. *Geo-phys. Res. Lett.*, 50(22), article no. e2023GL105292.

Lau, K. H., Louden, K. E., Funck, T., Tucholke, B. E., Holbrook, W. S., Hopper, J. R., and Christian Larsen, H. (2006). Crustal structure across the Grand Banks—Newfoundland Basin Continental Margin—I. Results from a seismic refraction profile. *Geophys. J. Int.*, 167(1), 127–156.

Lavier, L. L. and Buck, W. R. (2002). Half graben versus large-offset low-angle normal fault: Importance of keeping cool during normal faulting. *J. Geophys. Res.: Solid Earth*, 107(B6), article no. ETG-8.

Lavier, L. L. and Manatschal, G. (2006). A mechanism to thin the continental lithosphere at magma-poor margins. *Nature*, 440(7082), 324–328.

Lavier, L. L., Roger Buck, W., and Poliakov, A. N. (1999). Self-consistent rolling-hinge model for the evolution of large-offset low-angle normal faults. *Geology*, 27(12), 1127–1130.

Le Pichon, X. and Barbier, F. (1987). Passive margin formation by low-angle faulting within the upper crust: The northern Bay of Biscay margin. *Tectonics*, 6(2), 133–150.

Le Pourhiet, L., Burov, E., and Moretti, I. (2004). Rifting through a stack of inhomogeneous thrusts (the dipping pie concept). *Tectonics*, 23(4), article no. TC4005.

Le Pourhiet, L., Chamot-Rooke, N., Delescluse, M., May, D. A., Watremez, L., and Pubellier, M. (2018). Continental break-up of the South China Sea stalled by far-field compression. *Nat. Geosci.*, 11(8), 605–609.

Le Pourhiet, L., May, D. A., Huille, L., Watremez, L., and Leroy, S. (2017). A genetic link between transform and hyper-extended margins. *Earth Planet. Sci. Lett.*, 465, 184–192.

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