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1 retard uraninite (UO2) oxidation upon oxygen intrusion.
2 31 Ga, overlapping with the estimated age of intrusion.
3 n rates even with modest levels of saltwater intrusion.
4 cesses involved in the response to territory intrusion.
5 gers and inhibit UO2 reoxidation upon oxygen intrusion.
6 -like feature is consistent with sedimentary intrusion.
7  move on substrates that flow in response to intrusion.
8 oethite, but is partially remobilized by CO2 intrusion.
9 coincident with the large-scale Saharan dust intrusion.
10 tributed to metamorphism of coal by basaltic intrusion.
11 n indoor air contaminated through soil vapor intrusion.
12 ved understanding of the potential for vapor intrusion.
13  VOCs and (ii) temporal variability in vapor intrusion.
14 hat some seismic events are related to magma intrusion.
15 es of VOCs and temporal variability in vapor intrusion.
16  as a threat or agonistic call within 2 s of intrusion.
17 ighly aggressive manner when facing homecage intrusion.
18 use of potable water and mitigation of water intrusion.
19 ccurred at far-field sites shortly after the intrusion.
20 eparation at a ridge is accommodated by dyke intrusion.
21 hat explosive eruptions can also cause magma intrusion.
22 led adverse effects of CO2 leakage and brine intrusion.
23 ntrusion was followed by a series of smaller intrusions.
24  F, and Cs) in water samples within granitic intrusions.
25 hort time intervals by faulting and magmatic intrusions.
26 nd disruption of visual fixation by saccadic intrusions.
27 ignated spinocerebellar ataxia with saccadic intrusions.
28 rovince, from dominantly flood lavas to sill intrusions.
29 erian volcanism, and by coeval Ni-rich magma intrusions.
30 c metamorphic lithologies and large plutonic intrusions.
31 troposphere and lower stratosphere during PV intrusions.
32 ver O2 is supplied, for example, by episodic intrusions.
33 ds, especially those associated with layered intrusions.
34  from the stratosphere, associated with deep intrusions.
35 ospheric ozone concentration and subtropical intrusions account 65% of the co- variability (below 5
36 y dyking, provide strong evidence that magma intrusion achieves the majority of plate opening in this
37 ld underlie behavioral response to territory intrusion across species spanning a broad phylogenetic r
38                            Thus, suppressing intrusions affected emotional content.
39 croscopic theories-classical capillarity for intrusion and classical nucleation theory (CNT) for extr
40 rtifacts, the microscopic mechanism of water intrusion and extrusion in the pores, which are thermall
41 ; numerical models of plate separation, dyke intrusion and faulting require at least two distinct mec
42 crust, including volcanic construction, dyke intrusion and faulting.
43  because of both secular deformation and the intrusion and find that both would increase the Coulomb
44 lecular simulation and theory of adsorption, intrusion and freezing in porous silica.
45 n equation to describe the thermodynamics of intrusion and in-pore freezing.
46 astal nuclear sites resulting from predicted intrusion and inundation with oxic seawater.
47             The surgical procedure permitted intrusion and palatal repositioning of the implants.
48 ld moderate the relationship between illness intrusion and psychological adjustment, such that intrus
49 es of assessing both domain-specific illness intrusion and role importance in predicting psychologica
50 during continental breakup leads to magmatic intrusion and volcanism, yet our understanding of the lo
51 h as coastal flooding and erosion, saltwater intrusion and wetland degradation.
52 e restite compositions only, producing mafic intrusions and a pronounced compositional gap.
53 val classes, with no differentiation between intrusions and deliberations.
54  storage requires considering multiple small intrusions and multiple spatial scales, and our approach
55 , with moderately strong connections between intrusions and nightmares, being upset by reminders, and
56 l to other symptoms in the acute phase, with intrusions and physiological reactivity among the most c
57                                              Intrusions and physiological reactivity were central in
58 isms allowing people to control these memory intrusions and reduce their emotional impact.
59                                     Magmatic intrusions and volcanic eruptions are intimately related
60 t provided a list of factors affecting vapor intrusion, and the influence of some of these are explor
61 nd 1.5 [0.3] respectively) among flashbacks, intrusions, and avoidance of thoughts, with moderately s
62 his downregulation of activity during memory intrusions appears to disrupt momentary awareness of unw
63               We suggest that these vertical intrusions are associated with upward flow of warmer flu
64        Wells located within 5 km of granitic intrusions are at risk of containing high levels of [U]
65 tion of the transplanted hand, although such intrusions are commonly reported in amputees [5, 6].
66                   We find that lower-crustal intrusions are focused mainly into a narrow zone approxi
67 to true intakes for matches, exclusions, and intrusions, ASA24 performed well.
68 nal tree coring might be applicable in vapor intrusion assessment.
69  the spacing between them, and the degree of intrusion associated with them.
70 eptual and mathematical models of soil vapor intrusion assume that the transport of volatile organic
71 ss became channeled into a stable deep-water intrusion at 900- to 1,300-m depth, as aqueously dissolv
72  suggest either spatially varying stochastic intrusion at the ridge axis or, more likely, crystalliza
73 es in the levels of PTSD symptom clusters of intrusion, avoidance and hyperarousal are associated wit
74 iodic contamination suggested that transient intrusion, backflow, release of particulates, or sloughi
75             Remote sensing indicates that an intrusion began after eruption onset and caused severe (
76 st: 1) repeated emplacement of magma through intrusions below the caldera centre; 2) occasional later
77              Common features of beta-hairpin intrusion between the two DNA strands and nucleotide fli
78 nfluenced by remote water mass formation and intrusion, biological carbon remineralization, or both.
79                                          The intrusions brought dry and ozone rich air of stratospher
80                                Shallow magma intrusion builds subsurface reservoirs that are drained
81 L-H2b are sufficient in alerting NK cells to intrusion but fail to support NK restraint of viral infe
82  located within 5-10 km distance of granitic intrusions but do not show correlations with metamorphis
83 ous SSEs at Kilauea was directly preceded by intrusions but rather occurred during times of normal ba
84     Nonvolatile compounds do not cause vapor intrusion, but they still move with the groundwater and
85 ates cooperate to defend their range against intrusion by neighboring groups.
86 s during social interactions, and into which intrusion by others can cause discomfort.
87 a normal fault that promoted subsequent dyke intrusion by stress unclamping.
88                      People often respond to intrusions by suppressing their retrieval, excluding the
89  playback experiments simulating territorial intrusions by wild capuchin monkey (Cebus capucinus) gro
90  source, above which the potential for vapor intrusion can be considered negligible, were defined.
91                                        Vapor intrusion can be prevented by natural attenuation in the
92                                        These intrusions can be classified as 'exceptional events', wh
93 between La Nina and western US stratospheric intrusions can be exploited to provide a few months of l
94         Evidence suggests deep stratospheric intrusions can elevate western US surface ozone to unhea
95                                 These iconic intrusions can thus be interpreted as eruptive features
96 ering amounts of constant-rate magmatic dyke intrusion, can explain the great variety of fault offset
97 rom groundwater to indoor air-known as vapor intrusion-can be an important exposure pathway at hazard
98 e common interpretation procedure of mercury intrusion capillary pressure (MICP) measurement for nano
99 s obtained from X-ray tomography and mercury intrusion capillary pressure porosimetry, we define a di
100 rations more than doubled during the Saharan intrusion compared with non-Saharan.
101 rface and lead to water permeation and Na(+) intrusion, consistent with ion-toxicity in islet beta-ce
102 ne crystal rims shows that episodes of magma intrusion correlate temporally with recorded seismicity,
103 hermore, a decrease in pH resulting from CO2 intrusion could reactivate the adsorption of Se(IV) and
104 l is based on an analysis of the EPA's vapor intrusion database, which contains almost 2,400 indoor a
105  the far-field transport of the oil from the intrusion depth.
106 f magma supply, the timing of secondary dike intrusions differs from that of the aftershocks.
107 and Observing Satellite interferometric dike-intrusion displacement maps with continuous Global Posit
108  that the first of two shocks in a creep- or intrusion-driven swarm triggers the second, when this ne
109 r volcanoes with known typical extrusion and intrusion (dyke) volumes, the new methodology presented
110 Despite progress, important limitations with intrusion effects in low resolution 2D pillar-based meth
111                                              Intrusion elicited robust c-fos mRNA expression in both
112 cell groups contributes to the regulation of intrusion-elicited behavioral responses.
113                             Fewer and weaker intrusion events follow in the two springs after the 199
114 d shift in the number of Potential Vorticity intrusion events over the Pacific are evident.
115 th respect to hydrolysis after several water intrusion-extrusion cycles.
116            We review theoretical results for intrusion/extrusion and freezing in silica pores and dis
117  the underlying mechanisms governing mercury intrusion/extrusion experiments.
118 reased due to nanoscale confinement, and the intrusion/extrusion hysteresis is practically suppressed
119 gest that the most important features of the intrusion/extrusion process can be understood in terms o
120 biogeochemical cycle study and stratospheric intrusion flux at the surface are discussed.
121                                          The intrusion frequency has strong interannual variability d
122  two-fold increase and westward shift in the intrusion frequency over the Pacific Ocean, due to the c
123 nd S-cones, excluded an explanation based on intrusion from rod- and S-cone-driven responses.
124 and immediate rhizosphere to prevent sulfide intrusion from the surrounding sediment is critical for
125                                        Vapor intrusion from volatile subsurface contaminants can be m
126 g into other pathways and protects them from intrusions from those pathways.
127                   Because marine groundwater intrusion has been shown to increase during the summer,
128 ft axis outwards, indicating that axial dyke intrusion has been the primary mechanism of segment grow
129 arbon dioxide record better supports a magma-intrusion hypothesis, and suggests that injection of iso
130 orthern end of the Red Sea, and low nutrient intrusion in comparison with the southern end.
131     Here we show how a recent segmented dyke intrusion in the Baretharbunga volcanic system grew late
132 ments the first and longest case of seawater intrusion in the WKP, and also indicates significant pos
133           To predict the impact of saltwater intrusion in these environments, we must first gain a be
134 n of carbon release associated with volcanic intrusions in the North Atlantic Igneous Province.
135 ii, deforms by a combination of shallow dike intrusions in the rift zones and earthquakes along the b
136 ipping reflections generated by thermohaline intrusions in the uppermost 1000 meters of the ocean.
137 tients made substantial numbers of erroneous intrusions in their demonstrations, such as inappropriat
138 g evidence for strain accommodation by magma intrusion, in addition to slip along normal faults, duri
139 verall, and time-series analyses showed that intrusion incidence declined more quickly.
140 tual retrieval, we compared correct recalls, intrusions (incorrect recall of either items from prior
141 ribution, orientation, and dimensions of the intrusions indicate a globally isotropic extensional str
142 nd testosterone secretion; and 3) diminished intrusion-induced c-fos expression in select 5-HTergic b
143 nt oceanic phenomena, including thermohaline intrusions, internal waves, and eddies.
144  The intervention reduced reports of thought intrusion, interviewer ratings of anxiety, and emotional
145 n groundwater, and they pose a risk of vapor intrusion into buildings.
146 ant discharge to marine waters and saltwater intrusion into coastal aquifers.
147 sion and psychological adjustment, such that intrusion into highly valued roles would be the most psy
148 ersity is best conserved by minimizing human intrusion into intact and relatively unfragmented landsc
149 ea level rise is expected to cause saltwater intrusion into many historically freshwater ecosystems.
150 ms controlling both brackish water and CO(2) intrusion into shallow aquifers along fault zones.
151 f the synoptically driven warm and moist air intrusion into the Arctic as a primary contributing fact
152 ing it closer to the shelf and enhancing its intrusion into the East China Sea.
153 t with DNA phosphate groups, with polycation intrusion into the major and minor grooves dependent on
154 dimension of the proteins was inadequate for intrusion into the pores.
155                                        Virus intrusions into nondisinfected drinking water distributi
156 cian items in levels B4-5 represent isolated intrusions into otherwise in situ Chatelperronian deposi
157   Here, we estimate AGI incidence from virus intrusions into the distribution systems of 14 nondisinf
158                                        While intrusions into the South China Sea echoed the Pacific D
159 in persistent, quasi-stationary low-pressure intrusions into the subtropics of the CNP, accompanied b
160 cause of chronic sleepiness distinguished by intrusions into wakefulness of physiological aspects of
161  building pressure conditions during a vapor intrusion investigation program to provide an improved u
162 ncentrations in indoor air to evaluate vapor intrusion is complicated by (i) indoor sources of the sa
163 that remobilization of trace elements by CO2 intrusion is not a universal physicochemical effect.
164 fense by potential hosts against egg dumping intrusions is minimal.
165 riving the year-to-year variability of these intrusions is thus relevant for effective implementation
166 om groundwater to indoor air--known as vapor intrusion--is an important exposure pathway at sites wit
167 ted and that were excluded, 2) the number of intrusions (items reported but not consumed), and 3) dif
168 attern of contamination points to deep-ocean intrusion layers as the source and is most consistent wi
169 l thought to have been trapped in deep-ocean intrusion layers at depths of approximately 1,000-1,300
170 s including necessary magnitudes of basaltic intrusion, mixing and mobilization of coal and basalt, a
171        Simulations with the analytical vapor intrusion model "Biovapor" corroborated the low explosio
172  The proposed solution relies on a 1-D vapor intrusion model that incorporates a piecewise first-orde
173 ocesses, a three-dimensional numerical vapor intrusion model was used to simulate the degradation, mi
174  the physical understanding in current vapor intrusion models.
175                                    Territory intrusion modulated similar brain functional processes i
176 n conductivity are directly tied to seawater intrusion moving inland and traveling 11 miles against t
177             Thus, the long-held view is that intrusions must precede and feed eruptions.
178  echoed the Pacific Decadal Oscillation, the intrusion northeast of Taiwan decreased markedly before
179          We find that the dimensions of dike intrusions obey a power law analogous to the Gutenberg-R
180 e rifting episodes, we demonstrate that dike intrusions obey scaling relationships similar to earthqu
181 c data suggest that most of the Dabbahu dyke intrusion occurred in less than a week.
182 ion of factors including DNA bending and the intrusion of a probe residue.
183 ed by groundwater pumping caused the lateral intrusion of arsenic contamination more than 120 metres
184  very relaxed set of criteria to prevent the intrusion of bias, we developed a new set of unbiased ST
185 omalous literal translations, indicating the intrusion of Chinese lexical structures into English pro
186                                 The possible intrusion of CO2 into a given freshwater aquifer due to
187 upflow of deep-lying saline water, extensive intrusion of current Baltic Sea water, and substantial t
188 paper we focus on a second mechanism: upward intrusion of displaced brine or brackish-water into a sh
189              These effects may be related to intrusion of extracellular calcium since they were also
190                         The time lag between intrusion of fresh, hot magma and an ensuing eruption is
191 of thermogenic methane occurred owing to the intrusion of Gondwana coals by Toarcian-aged Karoo-Ferra
192       This has resulted in the unprecedented intrusion of government and the legal systems into the p
193 interactions, CO2 sequestration in rock, and intrusion of groundwater aquifers by saline water.
194 subtropical wave breaking events lead to the intrusion of high PV (potential vorticity) air along the
195 uorescent dye displacement assay confirm the intrusion of IL molecules into the DNA minor groove.
196                                          The intrusion of lead into the lens may alter lens redox sta
197 stant darkness and is influenced strongly by intrusion of light at night.
198        Experiments and modeling identify the intrusion of neuronal offline periods as a mechanism tha
199 ing in the north and wind-induced horizontal intrusion of nutrient-rich water in the south), and mini
200 re of all three domains has shifted with the intrusion of oil.
201            I. emarginata are able to prevent intrusion of particles even smaller than 1 mum into the
202 es for horizontal gene transfer, and enables intrusion of pathogenic organisms through depletion of o
203 jury, repair barrier function, and limit the intrusion of pathogenic organisms.
204  by overt retrieval or refractory access; 2) intrusion of perceptual information on semantic processi
205 provides the best example of the detrimental intrusion of politics into public health.
206 st that PCL recognition of H3K36me3 promotes intrusion of PRC2 complexes into active chromatin region
207 blems: inability to maintain wakefulness and intrusion of rapid eye movement (REM) sleep into wakeful
208 sleep-wake cycle with fluctuating vigilance, intrusion of rapid eye movement dream imagery into wakef
209 ness during waking that are thought to be an intrusion of rapid eye movement sleep muscle atonia into
210                     SP arises from anomalous intrusion of REM processes into waking consciousness, in
211 e receptor antagonist, reduces this abnormal intrusion of REM-like activity during wakefulness.
212           We find no evidence for persistent intrusion of representations of the face within the repr
213 ed and 'protecting' an active brain from the intrusion of resting state brain activity.
214  deeper sediments in situ by replicating the intrusion of shallow groundwater through injection of 1,
215         Several ecological changes allow the intrusion of sylvatic reservoirs and triatomines to the
216 of prior work yet simultaneously features an intrusion of unusual combinations.
217 iatric conditions that involve the automatic intrusion of unwanted memories.
218 nger than for water, which gives rise to the intrusion of urea into the protein interior and to urea'
219                  During this event, a strong intrusion of warm and moist air and an increase in downw
220 c sugar out of the helix and the concomitant intrusion of water into the interior of the helix.
221                                          The intrusion of water into the pores of hydrophobic materia
222                                          The intrusion of water into this region is slowed down by th
223                 This shift is accompanied by intrusion of water into Trp-cage's interior and the hydr
224  were subsequently pressured to minimize the intrusion of wildlife onto their farm fields by removing
225 thened Siberian High, which favors southward intrusions of cold air to East Asia and thus causes seve
226 duced false recall, with significantly fewer intrusions of critical items.
227 orming the upper parts of very deep magmatic intrusions of kimberlite rock.
228                 Helens that record pulsatory intrusions of new magma and volatiles into an existing l
229 also reveal previously unrecognized episodic intrusions of oxygen into the AMZ core, which could peri
230 g reveals that during the spring transition, intrusions of POC-rich surface water descend as coherent
231 ability to maintain wakefulness and abnormal intrusions of rapid eye movement sleep-related phenomena
232     Increased nuclear size and less frequent intrusions of the nuclear envelope into the nuclear lume
233 ity are reflected in patterns of territorial intrusion, offspring paternity, avpr1a expression, and t
234 ker and parent roles, the effects of illness intrusion on adjustment were moderated by whether respon
235 hwest Scotland we assess the impacts of salt intrusion on carbon accumulation rates.
236 rimental investigation of the effects of CO2 intrusion on the mobility of toxic ions in simplified eq
237                   There are two hot spots of intrusion, one in the Luzon Strait and the other off nor
238 rom northeast Taiwan, weakening the Kuroshio intrusion onto the East China Sea shelf.
239 ersistent contamination had occurred through intrusion or backflow.
240 mide (Br(-)) and iodide (I(-)) from seawater intrusion or high mineral content in the source waters.
241 e interpreted to be ancient vertical tabular intrusions or dikes formed by magmatism in combination w
242  to simulate the degradation, migration, and intrusion pathway of methane and benzene under different
243 re than 30 square-wave jerks (small saccadic intrusions) per minute, versus 0 to 8 in the control sub
244 ng the capillary pressure curve in a mercury intrusion porosimetry (MIP) measurement.
245      Comparisons have been made with mercury intrusion porosimetry and scanning electron microscopy i
246 niques over bulk measurements (e.g., mercury intrusion porosimetry).
247 rocarbon degradation, and increase the vapor intrusion potential for benzene.
248 -derived methane may also increase the vapor intrusion potential of toxic fuel hydrocarbons by stimul
249 iodegradation, thus increasing benzene vapor intrusion potential.
250 are reduced eightfold compared with CNT, the intrusion pressure is increased due to nanoscale confine
251            We demonstrate that a recent dike intrusion probably triggered a slow fault-slip event (SS
252                          Relative to the non-intrusion probe ERP, that to the intrusion probe was mor
253  to the non-intrusion probe ERP, that to the intrusion probe was more negative over frontal scalp (ap
254     The reaction time difference between the intrusion probe, a match of a to-be-rejected digit, and
255 match of a to-be-rejected digit, and the non-intrusion probe, which did not match any of the 4 digits
256 ter per year, similar to the amount of magma intrusion required to supply the observed high heat flow
257 hat the barotropic nature of the subtropical intrusions restricts the tracers within the UT.
258  that current approaches to manage the vapor intrusion risk for conventional fuel released might need
259 mends as a screening tool in assessing vapor intrusion risks.
260 ly interrupted by microsaccades and saccadic intrusions (SI).
261 ation; fixational eye movements and saccadic intrusions (SIs) continuously change the position of gaz
262 layer to sustain local defects such as water intrusions stresses the importance of going beyond mean
263           We review the high pressure forced intrusion studies of water in hydrophobic microporous ma
264 c carbon concentrations during surface water intrusion support heterotrophy, which succumbs to autotr
265 indings on a measure of clinical post-trauma intrusion symptoms at 1 week, but not on other symptom c
266  traumatization and an increased severity of intrusion symptoms may be related to hypocortisolism.
267  to be negatively related to the severity of intrusion symptoms, the number of different lifetime tra
268 d that the better people were at suppressing intrusions, the more it reduced their emotional response
269 the existing link between soil-gas and vapor intrusion, this study also indicates that directional tr
270 sion in olivine crystals, we constrained the intrusion-to-eruption time lag to between 3 and 10 weeks
271                                        These intrusions transcend multiple scales in time and space,
272 on account of the high pressure shift of the intrusion transition.
273 nd deformation, suggest that both extrinsic (intrusion-triggering) and intrinsic (secular fault creep
274                                        Vapor intrusion (VI) by volatile organic compounds (VOCs) in t
275 nmental Protection Agency (U.S. EPA)'s vapor intrusion (VI) database, there appears to be a trend sho
276 ns related to the investigation of TCE vapor intrusion (VI) in two houses.
277                                        Vapor intrusion (VI) investigations often require sampling of
278 lene (TCE) in indoor air in support of vapor intrusion (VI) investigations.
279                             A complete vapor intrusion (VI) model, describing vapor entry of volatile
280                                        Vapor intrusion (VI) pathway assessment and data interpretatio
281                                Current vapor intrusion (VI) pathway assessment heavily weights concen
282 bility of estimating the risk posed by vapor intrusion (VI) processes have often looked to informatio
283  the emerging public health problem of vapor intrusion (VI).
284                                  Thus, magma intrusion via dyking, rather than segmented normal fault
285 pths of 2 and 9 km, corresponding to a total intrusion volume of approximately 2.5 km3.
286  In both cases, the initial and largest dike intrusion was followed by a series of smaller intrusions
287                     For all 4 roles, illness intrusion was related to decreased psychological well-be
288 ns was sufficient to determine whether vapor intrusion was the primary source of VOCs in indoor air a
289                                The number of intrusions was higher in ASA24 (P < 0.01).
290 portantly, participants who did not suppress intrusions well showed increased negative affect, sugges
291 edented snapshots of the traceless bacterial intrusion were obtained using cryo-electron microscopy.
292         Beyond seasonal time scales, the two intrusions were not synchronous during 1993-2013.
293  impacted sites several months following oil intrusion when the highest concentrations of oil were pr
294 show more frequent late spring stratospheric intrusions when the polar jet meanders towards the weste
295 ere more likely to run away from territorial intrusions when their group had a numeric advantage; eac
296 erior cortical atrophy showed large saccadic intrusions whose frequency correlated significantly with
297 astal legacy nuclear sites to inundation and intrusion with oxygenated seawater.
298                                        Vapor intrusion would also be exacerbated if methanogenic acti
299  hypothesis, we hypothesized that 1) illness intrusion would predict psychological well-being and 2)
300 bination of mechanical deformation and magma intrusion, yet the spatial and temporal scales over whic

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