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1 atic activity (primary outgassing or contact metamorphism).
2 es in NWA 7983 record a high degree of shock metamorphism.
3 t exist at mantle depths associated with UHP metamorphism.
4 ngite ages reliably record the timing of UHP metamorphism.
5 ted objects subjected to thermal/accretional metamorphism.
6 been reported in association with high-grade metamorphism.
7 ions generated during ultra-high temperature metamorphism.
8 mation resulting from Pb mobilization during metamorphism.
9 ed, but even they have experienced low-grade metamorphism.
10 ying that the Os(i) carrier was destroyed by metamorphism.
11  typically thought to occur during low-grade metamorphism.
12 served within minerals that are resistant to metamorphism.
13 rved as crystalline graphite during prograde metamorphism.
14 at was accreted to the parent asteroid after metamorphism.
15                     Multistage mineralogical metamorphism affects the dynamic stability of megathrust
16 or providing insight into aspects of organic metamorphism and biochemical evolution, and for clarifyi
17 which porphyroblast minerals nucleate during metamorphism and carry implications for the role that no
18 ablish the timing and duration of magmatism, metamorphism and deformation.
19 0 km depth, marking the depth of dehydration metamorphism and eclogitization.
20  archive of diagenetic temperatures, despite metamorphism and exposure to meteoric fluids, and show t
21 ring late Archean ca. 2.9 Ga thermal contact metamorphism and not in an early ca. 3.45 Ga subseafloor
22  first continents that formed via high-grade metamorphism and partial melting of hydrated basaltic cr
23 f the crust strongly influences deformation, metamorphism and plutonism.
24              The progressive increase of ice metamorphism and re-crystallization with depth, favours
25 t in relationships between blueschist-facies metamorphism and seismicity, particularly through dehydr
26 the crystallization of magmas, fluid flow in metamorphism and the sealing of open cracks in earthquak
27 perienced high temperature-to-pressure ratio metamorphism and were most likely transported to deep ar
28 rt on an interpretation that eclogite-facies metamorphism and, therefore, collisional orogenesis, occ
29 s, a granoblastic calcite texture (incipient metamorphism), and subsequent hypidioblastic white mica
30 erates fast and very short orogeny, regional metamorphism, and exhumation.
31 oidal impacts and meteorite craters by shock metamorphism, and in Earth's mantle 1 to 2 billion years
32 ale mineralogical changes during diagenesis, metamorphism, and ore formation.
33 n their parent bodies, including alteration, metamorphism, and shock events.
34 n of heat by melt generates granulite facies metamorphism, and widespread andalusite-sillimanite meta
35 n and graphite precipitation occurred before metamorphism (approximately 2,665 Ma).
36         We evaluate the emergence of bimodal metamorphism (as a proxy for secular change in plate tec
37 ve aqueous alteration and subsequent thermal metamorphism at 570-670 K (300-400 C), suggesting that R
38 intrusions but do not show correlations with metamorphism at intermediate scales (10(0)-10(1) km).
39 mately400°C, it follows that parent body metamorphism cannot explain the absence of 26Mg* in some
40 tening, magmatism, and high thermal gradient metamorphism connected cratons in Australia, East Antarc
41 e Nimrod Complex indicate that high-pressure metamorphism did not occur in the Palaeoproterozoic, but
42  crust--for the localized nature of eclogite metamorphism during Caledonian crustal thickening, as re
43 very from the mantle through zones of active metamorphism eliminates the mass-balance argument for th
44 zed subgroup at a depth where fluid-assisted metamorphism enhanced the Na content.
45 tered-Fe domains and 1,412+/-56 Ma (tectonic metamorphism) from planar and subgrain boundary structur
46 ral changes due to chemical transport during metamorphism has been previously impossible both in natu
47 lite transition during burial diagenesis and metamorphism, impeding the maturation of organic materia
48 ata that dates the timing of eclogite facies metamorphism in eastern Papua New Guinea at 4.3 +/- 0.4
49  diagnostic features for high level of shock metamorphism in impact craters and meteorites.
50 igh monzodioritic proportion and inefficient metamorphism in the Breaksea Orthogneiss resulted in its
51 s constructed to probe the degree of thermal metamorphism in the crust in the effort to recreate the
52 phism, and widespread andalusite-sillimanite metamorphism in the upper crust.
53 he past two million years by intense crustal metamorphism induced by the Yellowstone hotspot.
54  trapped in minerals crystallized during UHP metamorphism is unknown.
55 tapped volatile-fertile sediments to contact metamorphism, likely liberating the massive greenhouse g
56 arbonaceous chondrite that experienced shock metamorphism, local melting (with conditions exceeding 5
57 metamorphic belts(5), which is attributed to metamorphism near (low T/P) and away from (high T/P) sub
58 n of CO2 and H2O through the subduction-zone metamorphism of carbonate-bearing marine sediments (whic
59 hane, which has primarily been attributed to metamorphism of coal by basaltic intrusion.
60 enozoic orogenesis are flawed, and that some metamorphism of Greater Himalayan rocks may have occurre
61 rom each planet's surface via the burial and metamorphism of hydrated mafic crusts, and calculate min
62                         It is known that the metamorphism of little-altered oceanic crust results in
63                                     The peak metamorphism of the garnet websterite was after approxim
64 ervation of prebiotic organic matter through metamorphism on Earth and beyond.
65  carbon could possibly confirm the effect of metamorphism on original biomass, but this is still unex
66 sure (thermobaric ratio) of granulite facies metamorphism peaked at over 1500 degrees C/GPa during th
67 ~4100 Ma dry melting and subsequent ~4070 Ma metamorphism provide new evidence for the diversity of t
68                                         Rock metamorphism releases substantial CO(2) over geologic ti
69                                 Late Archean metamorphism significantly reduced the kerogen's adsorpt
70  implications for revising traditional shock metamorphism stages.
71 o the mantle, where ultrahigh-pressure (UHP) metamorphism takes place.
72  a late Archean model age of 2610 Ma for the metamorphism that produced the nanospheres.
73                        Graphitization during metamorphism thus stabilizes carbon in the crust over ge
74  both the crystallization age and age of the metamorphism to ~+/-135 Ma, a significant improvement on
75 traditionally petrographic evidence of shock metamorphism - to resolve the debate.
76                                              Metamorphism, to the second sillimanite isograd, with ex
77  results indicate that impact-driven thermal metamorphism under low-pressure conditions led to partia
78 ted basalt) during high pressure/temperature metamorphism via phengite crystallization from subductio
79 y large sizes in Tissint indicate that shock metamorphism was widely dispersed in this sample (~25 GP
80 ise to extreme thermobaric ratios of crustal metamorphism when plate velocities were slowest.
81  that has experienced ultra-high temperature metamorphism, where ion imaging has revealed submicromet
82 lder than 3,500 Myr have experienced intense metamorphism, which would have obliterated any fragile m
83  reached 550 K, then fluids released by rock metamorphism would have promoted conditions favorable fo