排序方式： 共有9条查询结果，搜索用时 390 毫秒
1
1.
Crystallization of anatectic melts in high-temperature metamorphic terrains releases volatile-rich magmas that can be transported into adjacent lithologies. This study addresses the variations in the oxygen, boron and hydrogen isotopic composition of aplite-pegmatite dikes that formed during the crystallization of anatectic melts in regional high-temperature metamorphism on the island of Naxos, Greece, and propagated upward into the overlying sequences of metamorphic schist. The transport distance of these dikes was increased through a significant horizontal component of travel that was imposed by contemporaneous low-angle extensional shearing. Laser fluorination oxygen isotope analyses of quartz, tourmaline, garnet, and biotite mineral separates from the aplite-pegmatite dikes show a progressive rise in δ18O values with increasing distance from the core. Oxygen isotope fractionations among quartz, tourmaline, and garnet show temperature variations from > 700°C down to ∼400°C. This range is considered to reflect isotopic fractionation beginning with crystallization at high temperatures in water-undersaturated conditions and then evolving through lower temperature crystallization and retrograde sub-solidus exchange. Two processes are examined for the cause of the progressive increase in δ18O values: (1) heterogeneous δ18O sources and (2) fluid-rock exchange between the aplite/pegmatite magmas and their host rock. Although the former process cannot be ruled out, there is as yet no evidence in the exposed sequences on Naxos for the presence of a suitable high δ18O magma source. In contrast, a tendency for the δ18O of quartz in the aplite/pegmatite dikes to approach that of the quartz in the metamorphic rock suggests that fluid-rock exchange with the host rock may potentially be an important process. Advection of fluid into the magma is examined based on Darcian fluid flow into an initially water-undersaturated buoyantly propagating aplitic dike magma. It is shown that such advective flow could only account for part of the 18O-enrichment, unless it were amplified by repeated injection of magma pulses, fluid recycling, and deformation-assisted post-crystallization exchange. The mechanism is, however, adequate to account for hydrogen isotope equilibration between dike and host rock. In contrast, variations in the δ11B values of tourmalines suggest that 11B/10B fractionation during crystallization and/or magma degassing was the major control of boron geochemistry rather than fluid-rock interaction and that the boron isotopic system was decoupled from that of oxygen. 相似文献
2.
3.
T. Levi A. Salamon D. Bausch J. Rozelle A. Cutrell S. Hoyland Y. Hamiel O. Katz R. Calvo Z. Gvirtzman B. Ackerman I. Gavrieli 《Natural Hazards》2018,93(1):113-125
Among the activities developed under the framework of the Global Earthquake Model, the development of a global consequences database was included. This was defined with the objective of serving as public repository of damages and losses, occurred on different types of elements because of a selected list of earthquakes with epicentres at varying locations around the globe, but also to be used as a benchmark for the development of vulnerability models that capture specific characteristics of the building typologies in each country. The online earthquakes consequences’ database has information on 71 events where 16 of them occurred in the Latin America and the Caribbean Region. A complete and comprehensive review and data gathering process were developed for these selected earthquakes accounting for different aspects and dimensions that were considered of interest, besides the physical damage, such as casualties, socio-economic implications, damages and disruptions in critical facilities and infrastructures, together with the occurrence of secondary events triggered by the ground shaking such as landslides and tsunamis. When possible, the damage and casualties were geo-located using a standardized approach and included in the database. The contributions of the Latin America and Caribbean Region to the database were at the same time a challenge and an opportunity to collect, review, put together and standardize, up to a certain point, damage data of previous earthquakes additionally of being a step forward in the field of open data. 相似文献
4.
An earthquake swarm struck the North Tanzania Divergence, East African Rift over a 2 month period between July and September 2007. It produced approximately 70 M > 4 earthquakes (peak magnitude Mw 5.9), and extensive surface deformation, concurrent with eruptions at the nearby Oldoinyo Lengai volcano. The spatial and temporal evolution of the entire deformation event was resolved by Interferometric Synthetic Aperture Radar (InSAR) observations, owing to a particularly favorable acquisition programming of the Envisat and ALOS satellites, and was verified by detailed ground observations. Elastic modeling based on the InSAR measurements clearly distinguishes between normal faulting, which dominated during the first week of the event, and intermittent episodes of dike propagation, oblique dike opening and dike-induced faulting during the following month. A gradual decline in the intensity of deformation occurred over the final weeks. Our observations and modeling suggest that the sequence of events was initiated by pressurization of a deep-seated magma chamber below Oldoinyo Lengai which opened the way to lateral dike injection, and dike-induced faulting and seismicity. As dike intrusion terminated, silicate magma ascended the volcano conduit, reacted with the carbonatitic magma, and set off a major episode of explosive ash eruptions producing mixed silicate-carbonatitic ejecta. The rise of the silicate magma within the volcano conduit is attributed to bubble growth and buoyancy increase in the magma chamber either due to a temporary pressure drop after the termination of the diking event, or due to the dynamic effects of seismic wave passage from the earthquake swarm. Similar temporal associations between earthquake swarms and major explosive ash eruptions were observed at Oldoinyo Lengai over the past half century. 相似文献
5.
The infrared spectra of melanoidins which were prepared from galactose and neutral and basic amino acids (at various ratios) support in general the conclusion gained in Part I of this series. A striking resemblance in the IR spectra was obtained in melanoidins which were prepared from a high ratio of sugar to amino acids (Type 1). The imprint of the amino acids was observed only in type 2 melanoidins, which are enriched with amino acids. 相似文献
6.
7.
Yariv?HamielEmail author Vladimir?Lyakhovsky Yehuda?Ben-Zion 《Pure and Applied Geophysics》2011,168(12):2199-2210
Laboratory and field data indicate that rocks subjected to sufficiently high loads clearly deviate from linear behavior. Non-linear
stress–strain relations can be approximated by including third and higher-order terms of the strain tensor in the elastic
energy expression (e.g., the Murnaghan model). Such classical non-linear models are successful for calculating deformation
of soft materials, for example graphite, but cannot explain with the same elastic moduli small and large non-linear deformation
of stiff rocks, such as granite. The values of the third (higher-order) Murnaghan moduli estimated from acoustic experiments
are one to two orders of magnitude above the values estimated from stress–strain relations in quasi-static rock-mechanics
experiments. The Murnaghan model also fails to reproduce an abrupt change in the elastic moduli upon stress reversal from
compression to tension, observed in laboratory experiments with rocks, concrete, and composite brittle material samples, and
it predicts macroscopic failure at stress levels lower than observations associated with granite. An alternative energy function
based on second-order dependency on the strain tensor, as in the Hookean framework, but with an additional non-analytical
term, can account for the abrupt change in the effective elastic moduli upon stress reversal, and extended pre-yielding deformation
regime with one set of elastic moduli. We show that the non-analytical second-order model is a generalization of other non-classical
non-linear models, for example “bi-linear”, “clapping non-linearity”, and “unilateral damage” models. These models were designed
to explain the abrupt changes of elastic moduli and non-linearity of stiff rocks under small strains. The present model produces
dilation under shear loading and other non-linear deformation features of the stiff rocks mentioned above, and extends the
results to account for gradual closure of an arbitrary distribution of initial cracks. The results provide a quantitative
framework that can be used to model simultaneously, with a small number of coefficients, multiple observed aspects of non-linear
deformation of stiff rocks. These include, in addition to the features mentioned above, stress-induced anisotropy and non-linear
effects in resonance experiments with damaged materials. 相似文献
8.
9.
We present a formulation for mechanical modeling of the interaction between fracture and fluid flow. Our model combines the
classic Biot poroelastic theory and a damage rheology model. The model provides an internally consistent framework for simulating
coupled evolution of fractures and fluid flow together with gradual transition from brittle fracture to cataclastic flow in
high-porosity rocks. The theoretical analysis, based on thermodynamic principles, leads to a system of coupled kinetic equations
for the evolution of damage and porosity. A significant advantage of the model is the ability to reproduce the entire yield
curve, including positive and negative slopes, in high-porosity rocks by a unified formulation. A transition from positive
to negative values in the yield curve, referred to as a yield cap, is determined by the competition between the two thermodynamic
forces associated with damage and porosity evolution. Numerical simulations of triaxial compression tests reproduce the gradual
transition from localized brittle failure to distributed cataclastic flow with increasing pressure in high-porosity rocks
and fit well experimentally measured yield stress for Berea sandstone samples. We modified a widely used permeability porosity
relation by accounting for the effect of damage intensity on the connectivity. The new damage-permeability relation, together
with the coupled kinetics of damage and porosity evolution, reproduces a wide range of realistic features of rock behavior.
We constrain the model variables by comparisons of the theoretical predictions with laboratory results reporting porosity
and permeability variation in rock samples during isotropic and anisotropic loading. The new damage-porosity-permeability
relation enables simulation of coupled evolution of fractures and fluid flow and provides a possible explanation for permeability
measurements in high-porosity rocks, referred to as the “apparent permeability paradox.”
The text was submitted by the authors in English. 相似文献
1