23 novembre 2018, salle B-250, 14h30.
Models of plate tectonic processes and their interaction with the convecting mantle: magmatism, vertical movements and thermo-chemical structure
During this talk, I will present different results from 2D high-resolution numerical modeling of lithosphere/mantle-scale processes involving plate tectonics and convection in the Earth’s mantle at different scale. The talk will be subdivided into three themes that all employ this modeling technique.
1. Thermal subsidence of extensional basins in the presence of sublithospheric convection. Here, I present models of lithosphere extension above an asthenosphere mantle that is convecting with sufficient vigor to explain e.g. surface heat flow of old (‘steady state’) oceanic lithosphere. The models indicate that thermal subsidence in the presence of such convection can differ substantially from the well-known McKenzie model that only implicitly accounts for convective heat flow. For example, thermal subsidence can become strongly protracted, because the thermal boundary layer may become advected upwards during thinning and therefore transport more heat through the cooling lithosphere than in the case, where the thermal boundary layer is assumed at a constant depth (e.g. the McKenzie model). Furthermore, the presence of sublithospheric convection beneath a sedimentary basin also results in dynamic vertical movements in the order of 10-100 m at a time scale of 2-20 Myr. Such movements are a possible cause of stratigraphic cycles that are otherwise commonly attributed to glacial eustasy.
2. LIP formation as a consequence of rift-induced mantle overturn. Here, I present modeling results that provide yet another mechanism for anomalous magmatism such as that associated with LIP formation in the embryonic North Atlantic during the Paleocene/Eocene as well the protracted high degree of activity that followed and continues in Iceland today. Using thermomechanical modeling we show that the following line of events are physically plausible: Rifting along an old Caledonian suture with a mafic lower crust partly in eclogite facies may lead to rapid delamination of the mantle lithosphere. This again leads to a rapid, but not particularly voluminous phase of magmatism. The detached mantle lithosphere rapidly sinks into the lower mantle and induces a return flow due off lower mantle material into the upper mantle. If the lower mantle has elevated potential temperature relative to the upper mantle, the return flow is amplified by thermal buoyancy, and a partial overturn of the mantle is initiated. Within 6 Myr from onset of lithosphere delamination, hot lower mantle material rises to the base of the rifts and starts melting. This melt phase leads to fast production of large volumes of melt consistent with North atlantic LIP formation at 55 Ma. After this, lower mantle upwelling and melt productivity decreases, but still continues in the following time until the present, consistent with the long-lived melt anomaly of the North Atlantic and present day Iceland.
3. Syn-convergent extension and UHP exhumation in the D’Entrecasteaux Islands of the Woodlark Basin. In this part of the talk, I will briefly present a thermomechanical model for the exhumation of Ultra-High-Pressure (UHP) rocks in the young core complexes of the D’Entrecasteaux Islands that are situated just west of the oceanic Woodlark Basin. Plate kinematic constraints of the latter indicate that UHP exhumation was associated with North/South extension of at least 100 km since 4 Ma. This had led some authors to propose a mechanism of reverse subduction (eduction), where the Northern margin of the Australian continental plate was first subducted and then exhumed by normal motion along the former subduction plane. In the other hand, structural fabrics of the exhumed UHP units imply diapiric exhumation which however is at odds with the amount of extension required from plate kinematics. The model I here present shows that exhumation by reverse subduction led to ductile extrusion and diapir-like fabric, even though exhumation was largely driven by >100 km extension. The model further shows that despite continued convergence between the Australian and the Pacific plates, coeval extension due to the opening of the Woodlark Basin could have been accommodated by subduction further North in the New Britain trench, as subduction of the Australian margin was reversed.
Petersen, K., Armitage, J., Nielsen, S. & Thybo, H. Mantle temperature as a control on the time scale of thermal evolution of extensional basins. Earth and Planetary Science Letters 409, 61-70, (2015).
Petersen, K. D., Nielsen, S. B., Clausen, O. R., Stephenson, R. & Gerya, T. Small-Scale Mantle Convection Produces Stratigraphic Sequences in Sedimentary Basins. Science 329, 827-830, (2010).
Petersen, K. D., Schiffer, C. & Nagel, T. LIP formation and protracted lower mantle upwelling induced by rifting and delamination. Scientific Reports 8, 16578, (2018).
Petersen, K. D. & Buck, W. R. Eduction, extension, and exhumation of ultrahigh‐pressure rocks in metamorphic core complexes due to subduction initiation. Geochemistry, Geophysics, Geosystems 16, 2564-2581, (2015).