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The tectonomagmatic evolution of the southern Coast Mountains batholith, British Columbia reveals the relation of magmatic tempo, deformation, and relative plate motions which inform models for growth of continental crust and convergent plate dynamics. Magmatism in the southern batholith is episodic, derived primarily from the mantle, and reflects lower‐plate dynamics (Cecil et al., 2018, https://doi.org/10.1029/2018gc007874, 2021, https://doi.org/10.1130/ges02361.1). New field, structural, geochronologic, and geobarometric results from the southern batholith document three episodes of deformation, each spatially and temporally coincident with a high magmatic flux event (HFE). Sinistral faulting (<117–103 Ma) and penetrative deformation (110–90 Ma) occurred only within two distinct areas affected by a HFE at 114–102 Ma. Following a magmatic lull, crustal shortening occurred after 90 Ma and before 72 Ma within the region affected by a second HFE (85–70 Ma). After 70 Ma and before 53 Ma, >100 km of dextral slip occurred on the Coast shear zone and minor shortening affected 64–62 Ma plutons, overlapping with the 64–61 Ma HFE. Thus, at the crustal level exposed in the southern batholith, the timing and location of deformation is linked to magmatic tempo and the style of deformation varies through time. These results suggest that magmatic HFE modulate the timing and location of deformation while relative plate motions during HFE influence the style of deformation. Periods of deformation in batholiths may thus record high‐flux magmatic events and coeval plate motion but do not necessarily signal changes in plate motions. Plain Language Summary: Understanding how continents grow and the dynamics of plate motions relies on knowing the geologic history of convergent margins. Here we present new data on the evolution of a Late Cretaceous‐Paleogene convergent margin preserved in the southern Coast Mountains batholith in British Columbia. Magmatism in the southern batholith is episodic, derived primarily from the mantle, and reflects lower‐plate dynamics (Cecil et al., 2018, https://doi.org/10.1029/2018gc007874, 2021, https://doi.org/10.1130/ges02361.1). Our new results show that the southern batholith experienced three episodes of deformation, each one coincident with one of three high‐magmatic‐flux events. This pattern suggests that the timing and location of deformation here is linked to magmatic tempo and the style of deformation varies independently. Thus, we conclude that magmatic patterns modulate the tempo and location of deformation and that relative plate motions during episodes of high‐flux magmatism control the style of deformation. Periods of deformation in batholiths may thus record high‐flux magmatic events and coeval plate motion but do not necessarily signal changes in plate motions. Key Points: The location and timing of deformation and high‐flux magmatism coincide across the southern Coast Mountains batholith between ca. 115 and 50 MaHigh‐flux magmatism controls the timing and location of deformation; style of deformation reflects plate motion during high‐flux magmatismDextral slip exceeded 100 km on the intra‐arc Coast shear zone (<70–53) Ma and caused Salinian‐style repetition of the batholith [ABSTRACT FROM AUTHOR]

[1] New structural, paleomagnetic, and apatite (U-Th)/ He results from the continental margin inboard of the Queen Charlotte fault (~54 [degrees]N) delineate patterns of brittle faulting linked to transform development since ~50 Ma. In the core of the orogen, ~250 km from the transform, north striking, dip-slip brittle faults and vertical axis rotation of large crustal domains occurred after ~50 Ma and before intrusion of mafic dikes at 20 Ma. By 20 Ma, dextral faulting was active in the core of the orogen, but extension had migrated toward the transform, continuing there until

Alpine glaciers are efficient agents of erosion and capable of significantly modifying topography. Despite recent advances in theoretical and field studies that quantify glacial erosion processes, few studies have documented glacial erosion rates over long (>[10.sup.6] yr) or large (more than tens of kilometers) scales. We use apatite (U-Th)/He (AHe) and apatite fission track (AFT) cooling ages to address the late Miocene to Holocene erosion history across two 60-km-long transects of the heavily glaciated southern Coast Mountains, British Columbia. Observed AHe cooling ages from equal elevation samples range between 1.5 and 8 Ma and suggest that thick alpine glaciers resulted in a 16 km shift of the highest point in the topography in the past 1.5-4.0 m.y. We evaluated temporal and spatial variations in erosion rates using a three-dimensional thermal-kinematic model that predicted AHe and AFT ages at the surface for different erosion histories. Comparison of model predicted and observed cooling ages suggests an increase in erosion rates of as much as 300% over the past 1.5-7 m.y., coincident with the onset of glaciation of this range. Keywords: glacial erosion, apatite (U-Th)/He, numerical modeling, Coast Mountains, paleotopography.

Garnet Sm‐Nd ages and pressure–temperature–time (P–T–t) paths for pelitic and semipelitic metamorphic rocks in the Mount Waddington area constrain the relationship between metamorphism and high‐flux magmatism recently identified in the southern Coast Mountains batholith. Amphibolite facies metamorphism in this area occurred at 99–90, 80, and 72–65 Ma at varying conditions of ~3 to 8 kbar and ~450°C to 685°C, partly associated with high magmatic fluxes at 85–70 and 61–48 Ma. P–T–t paths indicate increases in pressure and temperature of 2 kbar and 120°C at c. 80 Ma and up to 3 kbar and 165°C at 72–65 Ma. Garnet growth at c. 72 and 80 Ma was synchronous with a high‐flux event at 85–70 Ma. However, c. 65‐, 90‐, and 99‐Ma garnet growth cannot be directly attributed to nearby plutons and occurred during lulls between high magmatic flux events. The simplest explanation for the observed P–T–t paths for metamorphism is a single regional‐scale event between 99 and 64 Ma, synchronous with and in response to crustal contraction. Rock textures and pressure–temperature (P–T) isochemical phase diagrams indicate that most sampled rocks reached near‐solidus conditions with little or no melting. Although partial melting of sedimentary rocks has been proposed to contribute toward high‐flux magmatism in the northern and central Coast Mountains, the timing of metamorphism and high‐flux events differs in the Waddington area, suggesting that they are unrelated. Therefore, we conclude that metamorphism and partial melting of rocks exposed at the current level of exhumation played little or no role in construction of the batholith in the Waddington–Raleigh area of the southern Coast Mountains batholith. [ABSTRACT FROM AUTHOR]

Examination of the history of deformation, plutonism and metamorphism reveals the evolution of the eastern Waddington thrust belt as an early Late Cretaceous northeast verging thrust belt. Mid-Cretaceous Coast plutonic arc is involved in the contraction and has provided heat for metamorphism. Radiometric, thermochronologic and structural data suggest that the thrust belt was active at 87 Ma and the occurrence of peak of postkinematic metamorphism between 82 and 84 Ma. Structured data reveal the involvement of synmagmatic contraction in the development of the arc.

Early Late Cretaceous east-vergent thrusts deform much of the eastern margin of the Coast Plutonic Complex in western British Columbia. Similarities in timing and style suggest that the faults represent a system of backthrusts to a west-vergent thrust belt on the west side of the complex. This geometry and the rarity of mid-Cretaceous strike-slip faults indicate that the Coast Plutonic Complex was a strongly contractional orogen in mid-Cretaceous time.

Alpine glaciation and river incision control the topography of mountain ranges, but their relative contributions have been debated for years. Apatite [sup.4]He/³He thermochronometry tightly constrains the timing and rate of glacial erosion within one of the largest valleys in the southern Coast Mountains of British Columbia, Canada. Five proximate samples require accelerated denudation of the Klinaklini Valley initiating 1.8 ± 0.2 million years ago (Ma). At [east 2 kilometers of overlying rock were removed from the valley at ≥ 5 millimeters per year, indicating that glacial valley deepening proceeded ≥ 6 times as fast as erosion rates before ~1.8 Ma. This intense erosion may be related to a global transition to enhanced climate instability ~1.9 Ma., The hypotheses that alpine glaciers erode at higher rates than rivers (1, 2) and control mountain topographic relief (3, 4) can be tested if pre- and syn-glacial erosion rates can [...]

This paper documents the newly recognized southern continuation of the early Tertiary Coast shear zone, extending its known length by ~350 km to more than 1200 km. Three sites along the shear zone in British Columbia, Douglas Channel, Bella Coola, and Machmell River, have similar histories during the period ca. 65-55 Ma. The shear zone is 2-11 km thick and is defined by well-developed mylonite zones that strike northwest and dip steeply northeast. Motion on the shear zone was predominantly reverse, with the northeast side up. Synkinematic plutons are common in the shear zone. Lower plate rocks, high-grade gneiss derived from an ancient continental margin assemblage, show little evidence of the extensive deformation and plutonism in the shear zone. North of Bella Coola, high-grade gneiss forms the upper plate, but to the south weakly metamorphosed rocks of Stikinia compose the upper plate, Geochronologic data show that the shear zone was active between ca. 60 and 55 Ma at Douglas Channel, ca. 62 and 56 Ma at Bella Coola, and after 66 and before 56 Ma near the Machmell River. These features match those of the Coast shear zone in southeast Alaska and adjacent British Columbia. Together the shear zones formed a continental-scale reverse ductile fault in Paleocene time. Plate reconstructions show an oblique component to the dominantly dextral transcurrent Paleocene margin. Partitioning of this motion across the continental margin produced a regional system of strike-slip faults and contraction on the Coast shear zone. Keywords: British Columbia, plutons, shear zones, tectonics, thrust faults.

Alpine glaciation and river incision control the topography of mountain ranges, but their relative contributions have been debated for years. Apatite [sup 4]He/³He thermochronometry tightly constrains the timing and rate of glacial erosion within one of the largest valleys in the southern Coast Mountains of British Columbia, Canada. Five proximate samples require accelerated denudation of the Klinaklini Valley initiating 1.8 ± 0.2 million years ago (Ma). At least 2 kilometers of overlying rock were removed from the valley at ≥5 millimeters per year, indicating that glacial valley deepening proceeded ≥6 times as fast as erosion rates before ∼1.8 Ma. This intense erosion may be related to a global transition to enhanced climate instability ∼1.9 Ma. [ABSTRACT FROM AUTHOR]