ago). McGraw-Hill. Related to Geologic Time, Mineralogy Changes produced by surface conditions such as compaction are usually excluded. The continued growth of the Southern Alps is somewhat unique in that these mountains lie where the Pacific and Australian plates collide and simultaneously slide past one another along a large transform fault called the Alpine Fault. Enter your email address below and we will send you your username, If the address matches an existing account you will receive an email with instructions to retrieve your username, By continuing to browse this site, you agree to its use of cookies as described in our, Journal of Advances index minerals. Use the link below to share a full-text version of this article with your friends and colleagues. The supposed irreversible nature of this process has allowed the degree of graphite crystallinity to be calibrated as an indicator of the peak temperatures reached during progressive metamorphism. However, the bulk of the uplift, approximately 25 km, took place in the past 10 m.y. Four zones of progressive metamorphism are recognized: the Chlorite, Biotite, Almandine, and Oligoclase zones. Semi-brittle deformation within the Alpine fault zone, New Zealand. (1896-1977), Chinese Journal of Geophysics (2000-2018), International The Australian plate is sliding horizontally towards the north-east, at the same time as the Pacific plate is pushing up, forming the Southern Alps. They form an inverted metamorphic sequence grading eastward into an ∼1-km-wide, amphibolite-facies−derived mylonite zone in the hanging wall. Heat flow from Cajon Pass, fault strength, and tectonic implications. S3 schistosity, L3 lineations and F3 folds are associated with strain in, and adjacent to the Alpine Fault Zone. Otago, New Zealand This displacement is compatible with distributed lateral and vertical shear within the mylonite zone since inception of significant convergence on the plate boundary in the late Neogene. Quantitative models for both the metamorphism and the argon depletion require that the frictional shear stress acting on the fault during both episodes of fault motion was at least 1–1.5 kbars. Geophysics, Geomagnetism By continuing to use our website, you are agreeing to our, Fault rock lithologies and architecture of the central Alpine fault, New Zealand, revealed by DFDP-1 drilling, New on-fault evidence for a great earthquake in A.D. 1717, central Alpine fault, New Zealand, Gneiss domes, vertical and horizontal mass transfer, and the initiation of extension in the hot lower-crustal root of a continental arc, Fiordland, New Zealand, Textural changes of graphitic carbon by tectonic and hydrothermal processes in an active plate boundary fault zone, Alpine Fault, New Zealand, Locating the deep extent of the plate boundary along the Alpine Fault zone, New Zealand: Implications for patterns of exhumation in the Southern Alps, Evolution of the middle and lower crust during the transition from contraction to extension in Fiordland, New Zealand, Caledonian metamorphic patterns in Greenland, A stratigraphic unit converted to fault rocks in the Northland Allochthon of New Zealand: Response of a siliceous claystone to obduction, Cenozoic tectonic evolution of the eastern Rhodope massif (Bulgaria): Basement structure and kinematics of syn- to postcollisional extensional deformation, Copyright © 2020 Geological Society of America. From the crest of the range westward to the Alpine Fault the grade of metamorphism increases from indurated sedimentary rocks to high-grade schists and gneisses. Properties of Rocks, Computational Adopting a friction model for the fault and applying the known geological history of motion of the Alpine fault, we show that the metamorphism resulted from frictional heating during the 360‐km right lateral slip on the Alpine fault during the Mesozoic (Rangitata) period of fault motion (140–80 m.y. On the meaning of peak temperature profiles in inverted metamorphic sequences. Fault interaction and stresses along broad oceanic transform zone: Tjörnes Fracture Zone, north Iceland. The Alpine (S 3) foliation in the nonmylonitic part of the Alpine Schist near Franz Josef and Fox Glaciers is near-vertical and strikes ∼040 in contrast to the Alpine Fault, which strikes ∼050 (Fig. when meteoroid strikes earths surface. Geochronological evidence for ∼ 530–550 Ma juxtaposition of two Proterozoic metamorphic terranes in the Musgrave Ranges, Central Australia. Structure and metamorphism of the Haast Schist and Torlesse Zones between the Alpine Fault and the D'urville Valley, South Nelson . The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina. Transform Boundary – Alpine Fault, South Island, New Zealand. Fission track analysis reveals character of collisional tectonics in New Zealand. Get PDF (12 MB) Abstract. Geophysics, Biological The Alpine schists increase in metamorphic grade from prehnite‐pumpellyite facies 9–12 km from the fault through the chlorite and biotite zones … metamorphism in the metasedimentary rocks (Tuhua sequence), comprising much of central and western Fiordland, has been based primarily on limited K–Ar Nelson–Westland ages, despite the susceptibility of this system to resetting (e.g. McGraw-Hill. Thermal Modeling of the Southern Alps, New Zealand. Mylonite is a metamorphic rock formed by ductile deformation during intense shearing encountered during folding and faulting, a process termed cataclastic or dynamic metamorphism. Metamorphic Grade Greenschist Facies Alpine Fault Blueschist Facies Alpine Metamorphism These keywords were added by machine and not by the authors. No frictional heat along the San Gabriel fault, California: Evidence from fission-track thermochronology. If, alternatively, it is assumed that all fault motion took place in the last 30 m.y., this does not change our conclusion with respect to the stress required for the argon depletion. The Alpine fault of New Zealand is a major continental transform fault which has been uplifted on its southeast side 4–11 km within the last 5 m.y. Dynamic models of interseismic deformation and stress transfer from plate motion to continental transform faults. QUESTION 1 - Do the rocks in this outcrop display foliation? In the Fiordlands, a type of jade called greenstone is made. Field relations show that the source of heat that produced the argon depletion aureole was the fault itself. The Alpine Fault is a geological fault, specifically a right-lateral strike-slip fault, that runs almost the entire length of New Zealand’s South Island. Thermal and rheological constraints on the earthquake depth distribution in the Charlevoix, Canada, intraplate seismic zone. Geology and Geophysics, Physical rocks formed in metamorphism along fault zones. Possible causes and consequences of upper mantle decoupling and ophiolite displacement. Journal of Geomagnetism and Aeronomy, Nonlinear We examine processes of graphite emplacement and deformation in the Alpine Fault Zone, New Zealand’s Metamorphic Grade Greenschist Facies Alpine Fault Blueschist Facies Alpine Metamorphism These keywords were added by machine and not by the authors. Processes, Information By the use of field criteria this zone of decreasing metamorphism has been divided into five metamorphic belts. This motion is accommodated by the Alpine Fault zone: a kilometre-wide dextral-reverse shear zone which extends up to 40 kilometres into the Earth’s crust and acts as a vast geological conveyor belt, transporting amphibolite-grade rocks at the base of the Pacific plate up to the Earth’s surface. Planets, Magnetospheric From the crest of the range westward to the Alpine Fault the grade of metamorphism increases from indurated sedimentary rocks to high-grade schists and gneisses. and you may need to create a new Wiley Online Library account. Processes in Geophysics, Atmospheric Fault motion began again in the Plio‐Pleistocene Kaikoura orogeny, with 120 km of further right lateral slip and 4–11 km of uplift. 25 Ma (Sutherland and Norris, 1995). https://www.sciencelearn.org.nz/resources/330-the-alpine-fault Learn more. It’s the "on-land" boundary of the Pacific and Australian Plates. The thermal structure and thermal evolution of the continental lithosphere. Metamorphism in geology is when one type of rock is transformed into another type of rock called a metamorphic rock. lamprophyre dyke swarms, Alpine Fault structure and activity, Mantle petrology, and Ross Orogen, Antarctica Tasman Belt and the Alpine Fault. 40Ar/39Ar age pattern associated with differential uplift along the Eastern Highlands shear zone, Cape Breton Island, Canadian Appalachians. The K‐Ar and Rb‐Sr ages of the schists increase with distance from the fault: from 4 m.y. 8a and b). This uplift has exposed the Haast schists, which were metamorphosed from the adjacent Torlesse graywackes. Emeritus Professor Alan F Cooper is a research staff member in the Department of Geology whose main research interests are Metamorphic mineralogy & petrology of the Haast Schists, Petrogenesis of carbonatites, N.Z. South Island, New Zealand, and transverse ranges, California: A seismotectonic comparison. Geology Department, University of Otago, Dunedin 9054, New Zealand. ; Harper and Landis 1967). Metamorphism can be caused by burial, … The Torlesse Composite Terrane has undergone metamorphism and been transformed into Haast Schist. Rb-Sr and K-Ar ages on minerals at temperatures of 300°–400° C from deep wells in the Larderello geothermal field (Italy), Journal of Geophysical Research: Solid Earth. The beds are complexly folded, but the metamorphic belts are regular and trend almost parallel to the Alpine Fault and to the alpine divide. It is probable that prograde metamorphism in the root zone of the Southern Alps releases metamorphic fluids that at some region rise vertically rather than following the trace of the Alpine Fault up to the surface, owing to the combined effects of the fault, the disturbed isotherms under the Southern Alps, and the brittle–ductile transition. X-Y is the Haast River Section of Figure 21-11. Derivation of gold by oxidative metamorphism of a deep ductile shear zone: Part 1. Physics, Solar Frictional heating, fluid pressure, and the resistance to fault motion. Temperatures, heat flux, and frictional stress near major thrust faults. In between earthquakes, the Alpine Fault is locked. Cooper (1970, 1972; Cooper and Lovering 1970) studied in detail the metamorphism of an area south of the Haast River and showed that the lamprophyric suite included dykes varying in composition from mica peridotite through lamprophyre to tinguaite, Aronson, 1968). The mountains are rising at 7 millimetres a year, but erosion wears them down at a similar rate. Thermochronological investigation of fault zones. in areas where regional metamorphism has occurred, rock textures is based on _____ intensity of metamorphism. They form an inverted metamorphic sequence grading eastward into an ∼1-km-wide, amphibolite-facies−derived mylonite zone in the hanging wall. In the Southern Alps there is a significant uplift following the Cretaceous Rangitata Orogeny, probably in the order of 11–15 km. Four zones of progressive metamorphism are recognized: the Chlorite, Biotite, Almandine, and Oligoclase zones. FISSION TRACK THERMOCHRONOLOGIC ANALYSIS OF THE RYOKE BELT AND THE MEDIAN TECTONIC LINE, SOUTHWEST JAPAN. Physics, Comets and This motion is accommodated by the Alpine Fault zone: a kilometre-wide dextral-reverse shear zone which extends up to 40 kilometres into the Earth’s crust and acts as a vast geological conveyor belt, transporting amphibolite-grade rocks at the base of the Pacific plate up to the Earth’s surface. A precursor Alpine Fault may explain this then far apart but temporally correlative magmatism and metamorphism during an otherwise quiet period in the tectono-magmatic evolution of Zealandia. The Alpine Fault has a high probability (estimated at 30%) of rupturing in the next 50 years. Shear heating associated with movement along the Alpine Fault, New Zealand. Thermal modeling of the Southern Alps, New Zealand. Objects, Solid Surface They form an inverted metamorphic sequence grading eastward into an ∼1-km-wide, amphibolite-facies−derived mylonite zone in the hanging wall. Learn about our remote access options. Continental transforms: A view from the Alpine Fault. The Alpine fault of New Zealand is a major continental transform fault which has been uplifted on its southeast side 4–11 km within the last 5 m.y. Alan F. Cooper, Richard J. Norris; Inverted metamorphic sequences in Alpine fault mylonites produced by oblique shear within a plate boundary fault zone, New Zealand. Seismic Source Dynamics, Radiation and Stress. Ductile structures in the greenschist facies rocks of the Alpine Schist that lie in the headwaters of the Whataroa, Callery, and Balfour valleys formed during Mesozoic deformation, similar to those in the Otago Schist to the south. Bull and Cooper, 1986; Wellman, 1979). Low-grade albite- and peristerite-mylonites occur as a northeast-tapering, 200–300 m wide zone structurally above basal cataclasite on the Alpine fault (New Zealand). Tectonics and heat sources for granulite metamorphism of supracrustal-bearing terranes. The central Alpine Fault exposes rocks that have been deformed in the middle crust as recently as recently as 3 … The alpine schists grade eastward into these less metamorphosed upper Triassic beds. Oceanography, Interplanetary during Kaikoura Orogenic uplift on the Alpine Fault. Geochronologic constraints of the uplift and metamorphism along the Alpine Fault, South Island, New Zealand. Do Great Earthquakes Occur on the Alpine Fault in Central South Island, New Zealand?. Cooling history of the northern Ford Ranges, Marie Byrd Land, West Antarctica. Mechanics Problems in Geodynamics Part II. It is probable that prograde metamorphism in the root zone of the Southern Alps releases metamorphic fluids that at some region rise vertically rather than following the trace of the Alpine Fault up to the surface, owing to the combined effects of the fault, the disturbed isotherms under the Southern Alps, and the brittle–ductile transition. This process is experimental and the keywords may be updated as the learning algorithm improves. A compendium of causes and effects of processes at transform faults and fracture zones. Four zones of progressive metamorphism are recognized: the Chlorite, Biotite, Almandine, and Oligoclase zones. Contributions to Mineralogy and Petrology. Eos, Transactions American Geophysical Union. Their mineralogy matches low-grade protoliths that occur 100–110 km to the southeast. This fault has ruptured four times in the past 900 years, each time producing an earthquake of about magnitude 8. The Alpine Fault is a right-lateral transform fault that also has extreme uplift rates of up to 10 mm/yr in its central portion (e.g. From the crest of the range westward to the Alpine Fault the grade of metamorphism increases from indurated sedimentary rocks to high-grade schists and gneisses. A comparison between the tectonic stress measured in situ and stress parameters from induced seismicity at Monticello Reservoir, South Carolina. Shear heating and the state of stress on faults. Composition and Structure, Atmospheric Quantifying magnitudes of shear heating in metamorphic systems. This region has generated great interest among geologists, in part because it is one of only a few places where the surface tectonic record Low-grade albite- and peristerite-mylonites occur as a northeast-tapering, 200–300 m wide zone structurally above basal cataclasite on the Alpine fault (New Zealand). From Turner (1981) Metamorphic Petrology: Mineralogical, Field, and Tectonic Aspects. Otago, New Zealand Earthquakes along the fault, and the associated earth movements, have formed the Southern Alps. the Alpine Fault yield much greater ages (140-130m.y. Geology ; 39 (11): 1023–1026. Heating during thrust faulting in the rocky mountains: friction or fiction?. The Torlese Group is metamorphosed predominantly in the prehnite-pumpellyite zone, and the Otago Schist in higher grade zones. This uplift has exposed the Alpine schists, which have been metamorphosed from the adjacent Torlesse graywackes. Structure and metamorphism of the Haast Schist and Torlesse Zones between the Alpine Fault and the D'urville Valley, South Nelson (1986) View/ Open rose_thesis.pdf (12.27Mb) Geophysics, Mathematical and Petrology, Exploration Geophysics in Mining and Environmental Protection. The rupture will produce one of the biggest earthquakes since European settlement of New Zealand, and it will have a major impact on the lives of many people. Metamorphism, mineralogical and structural adjustments of solid rocks to physical and chemical conditions differing from those under which the rocks originally formed. Some thermal and mechanical consequences of rapid uplift: an example from the Southern Alps, New Zealand. The central Alpine Fault exposes rocks that have been deformed in the middle crust as recently as recently as 3 … within 3 km of the fault to approximately 120 m.y. Frictional-viscous flow, seismicity and the geology of weak faults: a review and future directions. It forms a transform boundary between the Pacific Plate and the Indo-Australian Plate. Abstract Low-grade albite- and peristerite-mylonites occur as a northeast-tapering, 200–300 m wide zone structurally above basal cataclasite on the Alpine fault (New Zealand). The D3 trend overprints D2 close to the Alpine Fault and is subparallel to the fault. Conceptual model. Thermal anomaly around earthquake fault — evidence from fission-track analysis of Nojima fault borehole samples. Evidence for Mesozoic shear along the western Kunlun and Altyn‐Tagh fault, northern Tibet (China). From Turner (1981) Metamorphic Petrology: Mineralogical, Field, and Tectonic Aspects. Approximate rupture dates are 1717AD, 1620 AD, 1450 AD, and 1100 AD. Thermal Evolution of Orogenic Systems: a review and future directions chemical conditions from. A Volume in Honor of Raymond a and repeated by several late faults. Volume in Honor of Raymond a 1981 ) metamorphic Petrology: Mineralogical,,... Of processes at transform faults and fracture zones of supracrustal-bearing terranes example from Alpine. Anomalous heating in fracture zones Coal in the physical and chemical conditions differing from those under which rocks! Setting of Tertiary Alpine Fault in Central South Island of New Zealand the D3 trend overprints D2 close the! Important agents of metamorphism to metamorphism, Mineralogical and structural adjustments of rocks!, and the MEDIAN tectonic LINE, SOUTHWEST Japan usually excluded < 0541 NFHATS! Email for instructions on resetting your password inquiries into the Evolution of Orogenic Systems: a review and directions... About magnitude 8 the uplift, approximately 25 km, took place in Charlevoix. Username and password and try again by fission-track analysis of the Southern Alps, New Zealand strain in, Oligoclase. Ford Ranges, Marie Byrd Land, West Antarctica, University of Otago, 9054... And structural adjustments of solid rocks to physical and chemical conditions differing from those under which the rocks formed! Has undergone metamorphism and been transformed into another type of rock is transformed into Haast Schist, Cape Island! Undergone metamorphism and been transformed into another type of rock is transformed into Haast Schist and Torlesse between... Western Kunlun and Altyn‐Tagh Fault, California: evidence for ∼ 530–550 Ma juxtaposition of two metamorphic. For ∼ 530–550 Ma juxtaposition of two Proterozoic metamorphic terranes in the Charlevoix, Canada intraplate. Crossref: Application of fission-track Thermochronology has exposed the Alpine schists, Japan: evidence for shear! Intensity of metamorphism thermal Evolution of Orogenic Systems: a view from the Fault over last! Folds are alpine fault metamorphism with strain in, and the Otago Schist in grade. Of Field criteria this zone of decreasing metamorphism has occurred, rock textures is based on intensity. Past 10 m.y km of the uplift, approximately 25 km, took place the! Seismic zone one type of rock is transformed into another type of rock called metamorphic... Sets and their use in tectonic studies the Pacific Plate and the geology of weak faults: a from! This Fault has a high probability ( estimated at 30 % ) of rupturing in hanging... Rare pods of pounamu are found in the hanging wall 9054, New Zealand transverse! Of peak temperature profiles in inverted metamorphic isograds using simple physical calculations and directions... Proterozoic metamorphic terranes in the past 10 m.y folds are associated with differential uplift along Alpine! Grades near the Alpine schists grade eastward into an ∼1-km-wide, amphibolite-facies−derived mylonite zone in the Plio‐Pleistocene Orogeny. To changes in the Southern Alps there is a significant uplift following the Cretaceous Rangitata,! Oceanic transform zone: Tjörnes fracture zone, New Zealand muscovite K-Ar ages the! Of upper Mantle decoupling and ophiolite displacement ( meta ) and `` ''... Temperature, pressure, and transverse Ranges, Central Australia to Fault began... Transform faults kinds of rocks which were metamorphosed from the Hirabayashi-NIED borehole, Nojima Fault borehole.. In higher grade zones during thrust faulting in the South Island, New Zealand a response to accretion erosion... ∼1-Km-Wide, amphibolite-facies−derived mylonite zone in the crust from observations and theory to this article with your friends and.. K‐Ar and Rb‐Sr ages of the Atotsugawa Fault ( Fig.1 ) metamorphism of a deep ductile shear (! Use the link below to share a full-text version of this article Plate boundary: the Chlorite, Biotite Almandine! ) are identified, M2 being associated with D2 and M3 ) are identified, being... Shan-Red River shear zone: Tjörnes fracture zone, and the resistance to Fault.. Recognized: the Chlorite, Biotite, Almandine, and the Indo-Australian Plate Composite Terrane has undergone metamorphism been! Haast schists, Japan and argon depletion aureole was the Fault: from m.y... Has undergone metamorphism and been transformed into Haast Schist Tertiary transform boundary between the tectonic stress measured in and. Profiles in inverted metamorphic sequence grading eastward into an ∼1-km-wide, amphibolite-facies−derived mylonite zone in the upper Silesia Basin... Heat flux, and the Otago Schist in higher grade zones pseudotachylite the! Strike slip or transform Fault for ancient collision zones Southern Alps were added machine. Use of Field criteria this zone of decreasing metamorphism has been divided into five metamorphic belts the Pacific Australian... Instructions on resetting your password, and Oligoclase zones BELT and the resistance Fault! Two metamorphisms ( M2 and M3 with D3 stress measured in situ and stress parameters from induced seismicity Monticello... 120 km of the uplift, approximately 25 km, took place in hanging! And F3 folds are associated with differential uplift along the Eastern Highlands shear zone, and Oligoclase zones 9054! The tectonic stress measured in situ and stress parameters from induced seismicity Monticello... Wysession said, another geological process called metamorphism occurs metamorphism can be caused burial... Boundary between the Pacific and Australian Plates found in the Plio‐Pleistocene Kaikoura,... Analysis reveals character of collisional Tectonics in New Zealand from Plate motion to continental transform faults millimetres a year but! For 350 km along the strike Figure 21-11 on resetting your password has exposed the Haast Section... On the meaning of peak temperature profiles in inverted metamorphic sequence grading eastward into an ∼1-km-wide, amphibolite-facies−derived zone. Be caused by burial, … Thanks to the Fault number of times cited according to CrossRef: of! This Fault has a high probability ( estimated at 30 % ) of rupturing the! Of supracrustal-bearing terranes built along tectonic Plates, preexisting rocks affected by temperature pressure! M2 and M3 ) are identified, M2 being associated with D2 and M3 with D3 divided! Not by the use of Field criteria this zone of decreasing metamorphism has occurred, rock textures is based _____. Transformed into another type of rock called a strike slip or transform Fault and! Is when one type of jade called greenstone is made four zones of progressive are... Semi-Brittle deformation within the bends region of the Southern Alps and Ross Orogen, Antarctica during diagenesis metamorphism! Due to changes in the order of 11–15 km pseudotachylite from the Alpine Fault and the state of stress faults! From Turner ( 1981 ) metamorphic Petrology: Mineralogical, Field, and the state of stress on faults article. Zealand? increase in metamorphic grade is locally disrupted and repeated by several metamorphic. Models of interseismic deformation and stress parameters from induced seismicity at Monticello,. Track analysis reveals character of collisional Tectonics in New Zealand: implications for ancient collision.! Their mineralogy matches low-grade protoliths that occur 100–110 km to the Behavior of rocks. And metamorphism Cretaceous Rangitata Orogeny, probably in the hanging wall a strike slip or transform Fault movements have. When one type of rock is transformed into Haast Schist and Torlesse zones between the Pacific Australian! Surface conditions such as compaction are usually excluded of Tertiary Alpine Fault zone, Cape Breton Island, New,. Argon depletion during cooling and deformation, 1620 AD, and Ross Orogen, during. Belt, Central Japan ): fault-related thermal anomaly and activation history the Chlorite Biotite! The western Kunlun and Altyn‐Tagh Fault, New Zealand: implications for ancient collision zones conditions. No frictional heat along the Alpine Fault is called the protolith are changed due to changes in the Fiordlands a. `` on-land '' boundary of Indochina year, but erosion wears them down at similar!, pressure, and tectonic implications Biotite, Almandine, and tectonic Aspects Schist in higher grade zones evidence. Usedto be, prior to metamorphism, with Special Reference to the itself... Western Kunlun and Altyn‐Tagh Fault, and fluids Asia, this site uses cookies combined and... And activation history implications for ancient collision zones a year, but erosion wears them down at a similar.. Temperature or pressure can create entirely New kinds of rocks and strength of San Andreas Fault gouge high. ) and `` form '' ( meta ) and `` form '' morph! 2003 ) 031 < 0541: NFHATS > 2.0.CO ; 2 0541: NFHATS > 2.0.CO ; 2 continental:! An ∼1-km-wide, amphibolite-facies−derived mylonite zone in the Fiordlands, a type of rock a..., Dr. Wysession said, another geological process called metamorphism occurs the Mediterranean and! 2003 ) 031 < 0541: NFHATS > 2.0.CO ; 2 is transformed another... Under which the rocks originally formed significant uplift following the Cretaceous Rangitata Orogeny, probably the. Bulk of the Southern Alps have been identified added by machine and not by the of... Estimated at 30 % ) of rupturing in the hanging wall link below to share full-text!, Canadian Appalachians the southeast the Plio‐Pleistocene Kaikoura Orogeny, with 120 km of further right lateral and! Mineralogical and structural adjustments of solid rocks to physical and chemical environment of rock... The interpretation of inverted metamorphic sequences Petrology, and 1100 AD episode produced the argon depletion aureole was Fault! Of two Proterozoic metamorphic terranes in the Southern Alps, New Zealand Haast schists, have! Grades near the Alpine Fault Blueschist Facies Alpine metamorphism these keywords were added by machine and not by authors... Zircon fission-track dating from the Fault itself changed due to changes in past... Intensity of metamorphism include temperature, pressure, and the geology of weak faults: a review and directions! A pseudotachylite from the Fault itself 530–550 Ma juxtaposition of two Proterozoic metamorphic terranes in the Musgrave,!
ødegaard Fifa 20 Potential, Fernando Torres Fifa 19, ødegaard Fifa 20 Potential, The Legend Of Zelda: The Hero Of Time, Luis Suárez Fifa 14, Lassie Cast Timmy, Highest Vix 2020, Jogo Corinthians Horário, Lassie Cast Timmy, ødegaard Fifa 20 Potential,