ABSTRACT LXXIII, August 2004 n. 1:
Attilio Boriani
and Evelina Giobbi
- Does the basement of
western southern Alps display a tilted section through the continental crust?
A review and discussion
Abstract -
One of the most intriguing geo-petrological
problems of Central Alps is the meaning of the presence side by side in the
southalpine basement of a lower crustal unit, the Ivrea-Verbano Zone and an
upper crustal unit, the Serie dei Laghi separated by a ductile shear zone,
the Cossato-Mergozzo-Brissago (CMB) Line. This situation has been interpreted
as an «exposed continental section». In this paper a great part of the data
produced in the last thirty years are examined and discussed critically. However
the authors are well aware that their work is unfortunately not exhaustive
especially for what concerns the Ivrea-Verbano Zone on which an enormous amount
of papers has been produced. The idea of a tilted section of the lower Paleozoic
crust is criticized in favor of a model of a trans-tensional emplacement of
the Ivrea Verbano Zone.
Francesco Paolo Sassi, Bernardo Cesare, Claudio Mazzoli, Luca Peruzzo,
Raffaele Sassi and Richard Spiess - The
crystalline basements of the Italian eastern Alps: a review of the metamorphic
features
Abstract -
We briefly review the state of the art on the metamorphic evolution of
the crystalline basements of the Eastern Alps, with emphasis on the Italian
sector. For each of the main structural units, Penninic, Austroalpine and
Southalpine, we present a short outline followed by the most recent results
obtained by the research team of metamorphic petrology operating at the University
of Padova.
Marcello Franceschelli,
Giovanni Gianelli, Enrico Pandeli and
Mariano Puxeddu
- Variscan and Alpine metamorphic events in the
northern Apennines (Italy): a review
Abstract - The Northern Apennines consist of oceanic and continental Mesozoic-Tertiary
units thrust over the deepest Tuscan metamorphic units, including Paleozoic
successions. Tuscan metamorphic units underwent two Alpine tectono-metamorphic
deformation phases, and only pre-Carboniferous ones were subjected to polyphase
Variscan metamorphism. For the first Variscan phase with a Sudetian age of
328 ±5.3 Ma, the estimated P-T values are ~0.8 GPa and ~670°C; for the second
Variscan phase, P~0.4-0.5 GPa, T~530°C. These P-T conditions were attained
only in the Gneiss and Micaschist Complexes. In Larderello Micaschist C. and
Gneiss C., pre-Alpine andalusite and muscovite (285±11Ma) might be related
to a Late Variscan thermal event (third Variscan phase) with P=0.15-0.25 GPa
and T >550 °C. During the first Alpine compressional phase (27-20 Ma),
Mesozoic-Tertiary sediments were buried to a maximum depth of 40-55 km. Peak
pressure values ranged from 0.8 to 1.2 GPa for Verrucano metasediments (Tuscan
metamorphic units), with the exception of those on Giglio Island (1.0-1.5
GPa). The Schistes Lustrés of Gorgona show peak pressure values of 1.3-1.6
GPa, while the same rocks on the Argentario Promontory and Giglio Island are
in the range 0.6-0.85 GPa. For both units, temperatures varied from 300° to
420° C (450°- 480°C in the Massa Unit). Extensional tectonics began in the
early to late Miocene according to different models, caused very rapid exhumation
(rough estimates: 2.0-2.5 mm/yr for the Apuan units and 3.9-4.0 mm/yr for
the Schistes Lustrés of Gorgona) up to 10-15 km depth and produced a second
main folding metamorphic phase (14-12 Ma) with P=0.3-0.5 GPa and T=300°-370°C.
The distribution pattern of Al-silicates reveals that Tuscany is divided into
NW-SE trending narrow parallel zones. Metamorphic grade increases from an
eastern kaolinite-bearing zone to a central kyanite-bearing zone corresponding
to the Massa Unit-Larderello alignment and then shows a westward decrease
in the Punta Bianca-Elba areas. Similarly, non-metamorphic rocks show a rough
decrease in illite crystallinity (°D2Q increase) from west to east and from
the lower to upper tectonic units. In Southern Tuscany and in the Tuscan Archipelago,
Tortonian-Quaternary magmatism produced contact metamorphism and hydrothermal
alterations.
Vincenzo Festa, Antonia
Messina, Antonio Paglionico, Giuseppe Piccarreta and Alessandro Rottura - Pre-Triassic history recorded in the Calabria-Peloritani
segment of the Alpine chain, southern Italy. An overview
Abstract - Clockwise P-T-(t) trajectories are generally recorded in the pre-Triassic
basement rocks of the Calabria-Peloritani segment of the Alpine chain. Geochronological
data point to a synchronism of T-peak and emplacement of huge masses of granitoids
at about 300 Ma. Decompression and heat supply from the granitic intrusions
mark the transition from Barrovian to low P/high T metamorphism. When the
preserved characters allow to trace prograde trajectories, a strong P increase
and a moderate T increase, sometimes with T peak delayed relatively to the
P peak.
These features are consistent with orogenic evolution
in which crustal thickening in early- middle-Hercynian contractional stages was
followed by crustal thinning in late-Hercynian extensional stages.
Moreover, in the Calabria-Peloritani segment of the
Alpine chain, pre-Hercynian metamorphic and magmatic evidence also occurs.
Carlo Alberto Ricci, Rodolfo Carosi, Gianfranco Di Vincenzo, Marcello Franceschelli and Rosaria Palmeri - Unravelling the tectono-metamorphic evolution of medium-pressure rocks from collision to exhumation of the Variscan basement of NE Sardinia (Italy): a review
Abstract - The basement of NE Sardinia consists of magmatic-sedimentary sequences
affected by a polyphase deformation (D1, D2, D3
and D4)) and an increase in the metamorphic grade northwards, toward
the inner zone of belt. D1 is mainly detected in the low-grade
zone, while D2 is widespread in the basement but partitioned
into domains with prevailing folding in the southernmost areas and shearing
in the north-central part. D2 structures were later overprinted
by two main systems of open to tight folds. On the basis of the mineral assemblages
of pelitic and quartz-feldspathic rocks, six metamorphic zones have been distinguished.
From south to north they are: biotite, garnet, staurolite + biotite, kyanite
+ biotite, sillimanite + muscovite and sillimanite + K-feldspar. The P-T path
of different metamorphic zones is a typical clockwise one due to thermal relaxation
after a homogeneous thickening stage. The metamorphic peak is pre- to-syn
S2 in the garnet and staurolite zones, whereas in the sillimanite
zones it is essentially syn-S2. In biotite and garnet zones, both
the D1 and D2 stages of tectono-metamorphic evolution
can be documented. In the garnet zone, petrological evidence indicates that
from the S1 to the S2 mineralogical assemblage there
was an increase in temperature (up to 30°C), along with a decrease in pressure
(0.2-0.6 GPa). From the staurolite + biotite zone to the sillimanite + K-feldspar-zone,
the D1 phase is not clearly documented, and samples recorded only
the retrogressive path after the thermal climax. The field gradient is nearly
concave towards the temperature axis. This is a consequence of the diachronous
development of the main parageneses and fabrics in the six metamorphic zones
during the exhumation stage. An age of about 340 Ma, found on syn-S1
celadonite-rich white mica, is interpreted as the time of maximum thickening
stage in the garnet zone; ages of 315-320 Ma for syn-S2 muscovites
are attributed to the end of chemical re-equilibration of white mica during
the D2 stage. The emplacement of granitoids in the axial zone has
had no influence on the early exhumation of the lower crust, but the different
exhumation rate may be related to the transpressional tectonic regime which
affected NE Sardinia during Variscan orogeny.
Laura Gaggero, Luciano Cortesogno and Jean Michel Bertrand - The pre-Namurian basement of the Ligurian Alps: a review of the lithostratigraphy,
pre-Alpine metamorphic evolution, and regional comparisons
Abstract - The Pre-Namurian basement of the Ligurian Alps (southern External Pennides)
records evidence of poly-orogenic pre-Variscan (Ordovician), Variscan and
Alpine evolution. In the Briançonnais domain, bimodal volcanism (tholeiitic
to transitional basalts and acidic calc-alkaline volcanites) of Cambro-Ordovician
age (~500 Ma) possibly suggesting a continental rift phase is associated with
pelitic and psammitic sedimentary rocks and to large volumes of turbiditic
(?) metarenites. The sequence was intruded by Early Ordovician, S-type granitoids
and later metamorphosed from high-pressure amphibolite up to eclogite-facies
conditions. The cogenetic or exotic nature of the eclogites, which are associated
with migmatites and evolved through granulite facies conditions, is doubtful.
Later, the metamorphic sequence was intruded by large granitic bodies (from
monzogranites and granites to granodiorites, in the 470-460 Ma time span),
and by rare gabbros and basic to intermediate dykes. Large metarhyolite bodies
are likely coeval with the intrusive events. Finally, medium to low P, amphibolite
facies, Variscan (327 Ma) metamorphism and with km-scale megafolding affected
all the metamorphic and magmatic sequences. A small basement slice, considered
of pre-Piedmont provenance, with Alpine high-pressure overprint, preserves
sequences of metarhyolites, metaconglomerates, metapelites (garnet micaschists),
garnet–bearing marbles with minor metabasalts and serpentine schists. The
geodynamic pattern is compared with other neighbouring Palaeozoic terranes.
Marco Bruno, Bruno Messiga, Gisella Rebay and Marco Rubbo - High pressure coronites in the western Alps: a record of reaction pathways
Abstract - This paper, after a short review on the historical development of the
use of the term «corona texture» to indicate a layered mineral structure developed
at the contact between two reacting minerals, describes methods and problems
encountered in the study of coronitic rocks. Four well-known examples of high-and
ultrahigh-pressure coronitic rocks from the western Alps (Monviso and Zermatt-Saas
concerning eclogitized ophiolites and Monte Mucrone and Dora Maira concerning
eclogitized continental crust) are presented and discussed as case studies.
It is stressed out that the study of coronitic rocks
by means of classic microstructural and determination of chemical composition
of reactants and products coupled with more recent thermodynamic modelling and
mass-balance calculation enhance our understanding of reaction mechanisms, our
knowledge of the role played by fluids and our ability to determine accurate
P-T paths followed by rocks, involved in major tectonic processes.
Valeria Caironi, Annita Colombo and Annalisa Tunesi - Geochemical approach to characterization and
source identification of the protoliths of metasedimentary rocks: an example
from the southern Alps
Abstract - We compare here the geochemical characters of metasediments from two main
units of the Southern Alps (Serie dei Laghi and Orobic basement). Concerning
the protoliths of the paragneisses from Serie dei Laghi, the Th/Sc vs Zr/Sc
correlations indicate that they are mainly controlled by the composition of
their sources (likely diorites to granodiorites); their REE patterns are well
comparable to the average composition of continental arc wackes. The suggested
environment is a dissected continental arc on an active margin. For the Serie
dei Laghi metapelites (Scisti dei Laghi) the large compositional variations
and the wide spread in some parameters (Th 5-15 ppm, Th/U 1.4-4.8, Th/Sc 0.35-0.92,
La/Th 3.3-7.8, REEtot 149-248) suggest mixing in different proportions
of sediments from geochemically «undifferentiated» and from differentiated
igneous sources, with a variable contribution of recycled sediments enriched
in heavy minerals. The metasediments from the Orobic basement have a more
pelitic character and show the influence of old upper crustal materials (Th/U=
3.6-6.7). Their main geochemical characters are compatible with a passive
margin environment.
Supplemental Material
-
Caironi et al. (Fig.1).pdf
Caironi et al. (Tab. 1).pdf
Lauro Morten, Paolo
Nimis and Elisabetta Rampone - Records of mantle–crust exchange processes
during continental subduction–exhumation in the Nonsberg–Ultental garnet peridotites
(eastern Alps). A review
Abstract - In the Nonsberg-Ultental area (Tonale nappe), Grt-bearing peridotites
occur in high-P migmatitic gneisses
enclosing relics of eclogites. The peridotites record the transformation of
high-T Spl-lherzolites to coronitic
Grt+Spl-lherzolites to fine-grained Amph±Grt-peridotites. The transformation
is preceeded by LILE enrichment and intrusion of hot melts, and accompanied
by deformation, hydration, LILE enrichment and LILE/HFSE fractionation. High-P metamorphism of peridotites and eclogites
and early migmatization of the country gneisses were virtually coeval and
possibly isofacial. The peridotites may represent former mantle-wedge material
that was subducted and cooled due to incorporation in a crustal slab and then
metasomatized by hydrous fluids left after crystallization of leucosomes.
Possible directions for further work on this and other sectors of the Variscan
belt where broadly similar rock associations have been found are proposed.
Raffaele Sassi, Corrado
Venturini and Péter Árkai - The
boundary between the metamorphic and non- to anchi-metamorphic domains in
the Southalpine basement s.l. of the eastern southern Alps: a review
Abstract - The Southalpine basement in the Eastern Alps consists of thick metamorphic
mainly phyllitic sequences which formed within greenschist facies conditions,
and unmetamorphosed to very-low grade Paleozoic sequences in its easternmost
part (Palaeocarnic Chain).
Many authors tried to localize the boundary between the metamorphic and
non-metamorphic domains. Recent studies demonstrated, by means of KI (Kübler
Index) data, that the locations of this boundary given in the maps are
uncorrect, and that the boundary occurs more eastwards than previously
suggested, mainly in correspondence of the Val Bordaglia Line.
The present review critically summarizes all data existing in the literature
(Kübler Index, Árkai Index, vitrinite reflectance, Colour Alteration Index of
Conodonts, fluid inclusions) concerning the location of the eastern boundary of
the Hercynian metamorphism, and discusses the occurrence and possible
significance of a local Alpine overprint to the east of the Val Bordaglia Line.
Annamaria Fornelli, Giuseppe Piccarreta, Pasquale
Acquafredda, Francesca Micheletti and Antonio Paglionico - Geochemical fractionation in migmatitic rocks
from Serre granulitic terrane (Calabria, southern Italy)
Abstract - The Hercynian crustal section in the Serre (southern Italy) is about 20
km thick and includes sub-greenschist to granulite facies metamorphic rocks
which have been used to study chemical modifications during metamorphism and
migmatization. The rocks studied include: (1) Stilo phyllites and Mammola
paragneisses from the upper crustal metasediments; (2) migmatitic paragneisses
from the lower crustal segment that contain evidence for multi-stage melting
and different degrees of partial melting and extraction of melts. The upper
crustal rocks and the uppermost migmatites retain the composition of common
shales. Descending to the lower levels the migmatitic metapelites show modified
bulk compositions relative to common shales. The degree of chemical modification
increases towards the base of the investigated section. The bulk-migmatites
and the melanosomes show an enrichment in MgO, FeO*, TiO2, Al2O3,
MnO, Sc, Y, V, Cr and REE and a depletion in SiO2, K2O,
Na2O, CaO, Rb, P, U. In the lowermost migmatitic metapelites enrichment
of Th and Zr is also evident. Bulk migmatites have negative Eu anomaly which
is larger in the residua. The migmatites reflect: i) diverse protolith bulk
compositions, ii) the effects of hydrous melting and mica dehydration melting
producing both melts crystallizing in
situ and melts which were extracted, iii) a different degree of melting
and of separation melt-restite, iv) different effects of rehydration on cooling.
The overall geochemical features suggest that the lower migmatites were derived
from a source similar to the Stilo phyllites, and that the upper migmatites
from protoliths similar to the uppermost unmodified Stefanaconi paragneisses.
With these assumptions the major element geochemical fractionation between
restites, bulk migmatites and melts formed during the multi-stage partial
melting has been modelled.
Supplemental Material
-
Fornelli et al. (Table 1).pdf
Fornelli et al. (Table 2).pdf
Eugenio Piluso and Lauro Morten - Hercynian
high temperature granulites and migmatites from the Catena Costiera, northern
Calabria, southern Italy
Abstract - The deepest portion of a Hercynian lithospheric section is exposed in
the northern sector of the Catena Costiera, Calabrian-Peloritan Arc. The section
consists of migmatites and granulites derived from pelitic-arenaceous sequences,
of small volumes of granitoid rocks, of Spl-harzburgites and pyroxenites intruded
by metagabbros. The Hercynian P-T evolution of the migmatites and granulites
follows a clockwise trajectory. The prograde path, in the stability field
of sillimanite, reaches the metamorphic peak condition at 750-800°C and 0.9-1.0
GPa. The retrograde path is characterized by a decompression up to 0.5 GPa
and 600°C through two intermediate steps at 0.8 Gpa and about 800°C, and 0.6-0.7
Gpa at 650-700°C, respectively accompanied by a general retrogression under
lower amphibolite facies and successively under lower greenschist facies conditions.
The exhumation of deepest portion of the Hercynian lithospheric section to
middle crustal levels took place along HT extensional shear zones. The following
stages of exhumation under amphibolitic and greenschist facies conditions
were accommodated by LT shear zones, at the ductile-brittle transition. The
crustal sequence of the Catena Costiera is crosscut by unmetamorphosed basaltic
dyke dated at 120 ± 1.3 Ma. Therefore, the Alpine orogenesis did not overprint
the Hercynian lithospheric section of the Catena Costiera, except for the
brittle deformation event.
Franco Rolfo and Simona Ferrando - Selected case studies
in the high and ultrahigh pressure terranes of Dabie Shan and Sulu (China)
Abstract - A unique metamorphic terrane, the Dabie Shan and Sulu regions in east-central
China, is well known worldwide for the widespread occurrence of rocks with
ultrahigh pressure metamorphic (UHPM) overprint. Among the considered case
studies, the Zhujiachong quartz-eclogites and related metamorphic veins followed
a clockwise P-T path. The veins are considered to have formed before metamorphic
peak by prograde breakdown of lawsonite. The eclogitic peak, estimated at
ca. 2.4 GPa and 700 °C, is followed by a two-stage retrograde evolution. UHPM
talc-kyanite quartzite with the mineral association typical of «whiteschist»
has been found in Dabie Shan at Hualiangting. The geologic setting and trace
element geochemistry suggest that the whiteschist derived from a felsic dyke.
A minimum P of 2.6-2.7 GPa and a T of ca. 710 °C have been estimated for the
metamorphic peak. The identification in Dabie Shan of a E-W trending narrow
belt ca. 40 km long and 1-2 km wide, the Wuhe-Pailou Unit (WPU), supports
the «in-situ» origin of the UHPM, and constrains the real size of the exhumed
tectonic units. A clockwise P-T path was inferred for the WPU, which consists
of an early prograde part up to P ~ 3.3 GPa and T ~ 720 °C and a two-stage
retrograde evolution. In southern Sulu, at Donghai, kyanite-phengite-epidote
eclogite and kyanite – OH-rich topaz quartzite were subjected to UHPM at P
~ 3.5 GPa and T ~ 850 °C. The growth of hydrous and/or zoned minerals under
eclogite facies conditions is promoted by brines with variable salinity and
type of dissolved cations ± CO2. The presence of high-density brines
at the coesite to quartz transition is also suggested by the primary fluid
inclusions within OH-rich topaz and by the related isochore that indicates
P = 2.8 GPa at 800 °C. Considerable differences in peak metamorphic P have
been recorded by quartz- and coesite eclogites in Dabie Shan and Sulu, but
the shape of post-peak P-T paths, characterized by a significant decompression
coupled with minor cooling, seems to be peculiar of all studied units.
Franco M. Talarico,
Rosaria Palmeri and Carlo Alberto
Ricci - Regional
metamorphism and P-T evolution of the Ross Orogen in northern Victoria Land
(Antarctica): a review
Abstract - The main focus of this paper is on
the petrological evolution of medium- to high-grade metamorphic units
in the Wilson Terrane, the westernmost lithotectonic unit of the Ross Orogen
in northern Victoria Land. The petrological data set is reviewed for all areas
where P-T-t paths have been reconstructed and geochronological data are sufficiently
complete to provide an overview of the regional metamorphic evolution of a
ca. 600 km long segment of the Ross
Orogen, from its termination along the Pacific coast to the Eisenhower Range
near the Ross Sea coast.
Petrological evidence reveals that different
lithological units of the Wilson Terrane equate with distinct lithotectonic
metamorphic complexes with partly independent P-T-t histories. In spite of the
wide range of estimated peak metamorphic conditions, and variability in both
shape of the P-T path (clockwise or counter-clockwise) and type of retrograde
evolution (isobaric cooling or cooling/unloading), the reviewed P-T-t
trajectories consistently support a setting of evolving subduction and
accretion in the context of a Palaeozoic cordilleran-type active margin.
Patrizia Fumagalli and Stefano Poli - Modelling metamorphic rocks in complex systems:
present-day developments in high pressure experimental petrology
Abstract - Metamorphic processes at subduction zones are strictly related to the
transfer and release of water via dehydration reactions from the subducting
slab toward the mantle wedge. Results and present-day developments in high
pressure experimental petrology in the laboratory of Milano are presented
here, dealing with lithologies which are expected to be subducted, i.e. mainly
mafics and ultramafics. Particular emphasis will be given to hydrate-bearing
assemblages.
Experiments performed in mafic rocks at pressures of
up to 5 GPa show that phase relationships are controlled by amphibole s.s. to
2.5 GPa and by epidote group minerals and lawsonite at higher pressure. Phase
relationships point out to strong sensitivity of assemblages from continuous
reactions and therefore from bulk composition considered.
In ultramafics, at temperatures between 680 and 800°C,
amphibole and chlorite are the major hydrous phases able to transport water
deep into the Earth’s Mantle. At pressure > 4.8 GPa, a hydrous silicate with
a 10Å phase structure forms at the expense of chlorite, providing a «carrier»
by which water might be transported down to 200 km depth. The interaction
between alkali-rich fluids and mantle peridotites lead to the occurrence of
potassic hydrous phases such as phlogopite. Experiments on K-peridotite suggest
a pressure dependent relevance of a «talc» component in phlogopites.
Maria Luce Frezzotti,
Bernardo Cesare and Marco Scambelluri - Fluids
at extreme P-T metamorphic conditions: the message from high-grade rocks
Abstract - The study of fluid inclusions in rocks which experienced extreme P-T metamorphic
conditions can provide valuable information on the composition of peak fluids,
to some extent on their origin, and on fluid-rock interactions which take
place in the lithosphere. A review is given, on the basis of the authors’
experience, of the major results obtained by fluid inclusions studies in the
fields of high pressure and ultrahigh pressure metamorphic rocks (eclogites),
high temperature and ultrahigh temperature metamorphic rocks (migmatites and
granulites), and high temperature and pressures mantle rocks.
Marco Scambelluri and Pascal Philippot - Volatile and mobile element recycling during
subduction of the oceanic lithosphere. Insights from metasediments and serpentinites
of the Alps
Abstract - We discuss some aspects of the release of light elements and volatile
components during subduction of serpentinite and metasedimentary systems.
Enrichment in B, Cl, and Sr during serpentinization of the oceanic mantle
is followed by their progressive release in the subduction fluids. Olivine–orthopyroxene
rocks formed after significant serpentinite dehydration still contain bulk
B, Cl and Li considerably higher than in mantle reservoirs and may introduce
light element anomalies into the upper mantle. The high to ultrahigh pressure
metasediments underwent little or no devolatilization, nor N release, down
to at least 90 km, acting as closed systems to the infiltration of externally
derived fluids. They therefore reflux to the mantle appreciable amounts of
exogenic N. This behaviour is supported by the oxygen isotope geochemistry
of high and ultrahigh pressure rocks, showing closed system behaviour and
limited fluid mobility at these depths. Many high pressure rocks thus do not
represent the levels of fluid extraction from slabs; we suggest that the antigorite
breakdown may represent a dehydration reaction creating a mobile, trace element-enriched,
subduction fluid.
Alessandro Borghi and Richard Spiess - Studying
metamorphic microstructures: a brief insight on modern methodological approaches
Abstract - Microstructures evolve in response to processes that rocks undergo during
their residence time in the Earth crust and mantle. For a thorough understanding
of microstructures all their critical aspects need to be analysed. Much of
the recent advances in the comprehension of microstructures and the interrelated
processes is linked to the advent of modern instrumental equipments as electron
and proton microprobes (EMPA, mPIXE) and to novel analytical techniques as
electron backscatter diffraction (EBSD) and orientation contrast imaging (OC).
In this review we highlight the basic concepts and the potential applications
of such modern analytical tools in microstructural analysis of metamorphic
rocks.
Maria Iole Spalla and Michele Zucali - Deformation vs. metamorphic re-equilibration heterogeneities in polymetamorphic
rocks: a key to infer quality P-T-d-t path
Abstract - The interaction between fabric gradients and reaction rate as a tool for
individuating volumes carrying the longest «rock memory» is discussed through some examples from continental
units of the Alpine chain. Here quality P-T-d-t paths have been inferred using
a sampling strategy based on reconstruction of the metamorphic evolution,
supported by a regionally valid deformation history and on the choice of sites
for investigations on compositional variations, where mineral growth and sequences
of overprinting fabrics are known. The examples show that correlation between
degree of fabric evolution and progress of metamorphic transformation is positive
and influence of strain partitioning on tectono-thermal rock memory must be
taken into account during P-T-d-t reconstruction to avoid errors in determining
the sequence of P-T re-equilibration steps and to obtain clustered P-T estimates
relative to each step.
Supplemental Material
-
Spalla_and_Zucali(Fig.01).pdf;
Spalla_and_Zucali(Fig.06).pdf;
Spalla_and_Zucali(Fig.07).pdf;
Igor M. Villa
- Geochronology of metamorphic
rocks
Abstract - Metamorphic minerals are formed at moderate to high depth in the Earth’s
interior. Those that have been subsequently exhumed to the Earth’s surface
are those that survived metastably outside their stability fields. The majority
of studied metamorphic rocks did not survive unscathed, and contains diachronic
mineral assemblages that record a plurality of P-T-A-X conditions along the
exhumation path, rather than a single P-T-A-X point that includes all minerals
in that rock. Such mixed assemblages are in mutual disequilibrium. Dating
a metamorphic event therefore requires great interpretive caution. While an
apparent age always results from mathematical equations, translating a number
into a geological interpretation can be ambiguous and requires establishing
a context among different isotope systems, and even more importantly, between
the isotope record and mineralogy, microtextures, and microchemistry. Electron
microscopy reveals that many minerals consist of mixtures at the sub-µm scale,
as they are intergrown with their retrogression products, and/or contain unequilibrated
relics (e.g. zircons, monazites, amphiboles, micas). Lack of chemical homogeneity
means that diffusivity under anhydrous conditions is extremely low. Modern,
direct determinations of dry diffusion in minerals yield rates that are orders
of magnitude slower than what was thought twenty years ago. If recrystallization
is incomplete, petrographic relics ensure isotopic inheritance. By contrast,
water accelerates recrystallization and so enhances element and isotope reequilibration,
both in experiments and in natural systems. Availability of water, not temperature,
is the principal factor controlling isotope transport. The isotope record
of a mineral is thus a geohygrometer and can be used, but only in connection
with petrological constraints, to reconstruct a rock’s petrogenetic path.