Thermal regime of the Costa Rican convergent margin: 1. Along-strike variations in heat flow from probe measurements and estimated from bottom-simulating reflectors

21 pages, 9 figures, 1 tableThe thermal structure of convergent margins provides information related to the tectonics, geodynamics, metamorphism, and fluid flow of active plate boundaries. We report 176 heat flow measurements made with a violin bow style probe across the Costa Rican margin at the Middle America Trench. The probe measurements are collocated with seismic reflection lines. These seismic reflection lines show widespread distribution of bottom-simulating reflectors (BSRs). To extend the spatial coverage of heat flow measurements we estimate heat flow from the depth of BSRs. Comparisons between probe measurements and BSR-derived estimates of heat flow are generally within 10% and improve with distance landward of the deformation front. Together, these determinations provide new information on the thermal regime of this margin. Consistent with previous studies, the margin associated with the northern Nicoya Peninsula is remarkably cool. We define better the southern boundary of the cool region. The northern extent of the cool region remains poorly determined. A regional trend of decreasing heat flow landward of the deformation front is apparent, consistent with the downward advection of heat by the subducting Cocos Plate. High wave number variability at a scale of 5–10 km is significantly greater than the measurement uncertainty and is greater south of the northern Nicoya Peninsula. These heat flow anomalies vary between approximately 20 and 60 mW m−2 and are most likely due to localized fluid flow through mounds and faults on the margin. Simple one-dimensional models show that these anomalies are consistent with flow rates of 7–15 mm yr−1. Across the margin toe variability is significant and likely due to fluid flow through deformation structures associated with the frontal sedimentary prismThis research was support by an NSF award (OCE‐0637120) to R.N.H. We thank R. von Huene, P. Fulton, and G. Spinelli for helpful comments. Heat flow data acquisition was funded by the German Science Foundation (DFG) through grant Vi 133/7‐1 to H.V. and I.G. and the SFB 574 “Volatiles and fluids in subduction zones” at Christan‐Albrechts University, Kiel. This is a contribution of the Barcelona Center for Subsurface Imaging (Barcelona‐CSI) supported by the Kaleidoscope project of REPSOLPeer Reviewe

Thermal regime of the Costa Rican convergent margin: 1. Along-strike variations in heat flow from probe measurements and estimated from bottom-simulating reflectors

The thermal structure of convergent margins provides information related to the tectonics, geodynamics, metamorphism, and fluid flow of active plate boundaries. We report 176 heat flow measurements made with a violin bow style probe across the Costa Rican margin at the Middle America Trench. The probe measurements are collocated with seismic reflection lines. These seismic reflection lines show widespread distribution of bottom‐simulating reflectors (BSRs). To extend the spatial coverage of heat flow measurements we estimate heat flow from the depth of BSRs. Comparisons between probe measurements and BSR‐derived estimates of heat flow are generally within 10% and improve with distance landward of the deformation front. Together, these determinations provide new information on the thermal regime of this margin. Consistent with previous studies, the margin associated with the northern Nicoya Peninsula is remarkably cool. We define better the southern boundary of the cool region. The northern extent of the cool region remains poorly determined. A regional trend of decreasing heat flow landward of the deformation front is apparent, consistent with the downward advection of heat by the subducting Cocos Plate. High wave number variability at a scale of 5–10 km is significantly greater than the measurement uncertainty and is greater south of the northern Nicoya Peninsula. These heat flow anomalies vary between approximately 20 and 60 mW m−2 and are most likely due to localized fluid flow through mounds and faults on the margin. Simple one‐dimensional models show that these anomalies are consistent with flow rates of 7–15 mm yr−1. Across the margin toe variability is significant and likely due to fluid flow through deformation structures associated with the frontal sedimentary prism

Thermal regime of the Costa Rican convergent margin: 1. Along‐strike variations in heat flow from probe measurements and estimated from bottom‐simulating reflectors

The thermal structure of convergent margins provides information related to the tectonics, geodynamics,\ud metamorphism, and fluid flow of active plate boundaries. We report 176 heat flow measurements\ud made with a violin bow style probe across the Costa Rican margin at the Middle America Trench. The\ud probe measurements are collocated with seismic reflection lines. These seismic reflection lines show widespread\ud distribution of bottom‐simulating reflectors (BSRs). To extend the spatial coverage of heat flow\ud measurements we estimate heat flow from the depth of BSRs. Comparisons between probe measurements\ud and BSR‐derived estimates of heat flow are generally within 10% and improve with distance landward of\ud the deformation front. Together, these determinations provide new information on the thermal regime of\ud this margin. Consistent with previous studies, the margin associated with the northern Nicoya Peninsula\ud is remarkably cool. We define better the southern boundary of the cool region. The northern extent of the cool region remains poorly determined. A regional trend of decreasing heat flow landward of the\ud deformation front is apparent, consistent with the downward advection of heat by the subducting Cocos\ud Plate. High wave number variability at a scale of 5–10 km is significantly greater than the measurement\ud uncertainty and is greater south of the northern Nicoya Peninsula. These heat flow anomalies vary between\ud approximately 20 and 60 mW m−2 and are most likely due to localized fluid flow through mounds and\ud faults on the margin. Simple one‐dimensional models show that these anomalies are consistent with flow\ud rates of 7–15 mm yr−1. Across the margin toe variability is significant and likely due to fluid flow through\ud deformation structures associated with the frontal sedimentary prism