ライフサイエンスコーパス: tectonic

1 ago, requiring an early initiation of plate tectonics.

2 , where it can significantly influence plate tectonics.

3 processes, crustal heterogeneity and active tectonics.

4 understanding of mantle convection and plate tectonics.

5 the context of changing weather, climate and tectonics.

6 n self-sustained subduction and global plate tectonics.

7 st subduction zone without the help of plate tectonics.

8 akness, which are both consequences of plate tectonics.

9 amental to understanding the origin of plate tectonics.

10 udes while in turn being influenced by plate tectonics.

11 he asthenosphere, is a requirement for plate tectonics.

12 er time led to an abrupt transition to plate tectonics.

13 tion of our planet before the onset of plate tectonics.

14 eat-pipe volcanism after initiation of plate tectonics.

15 nked to the onset of subduction-driven plate tectonics.

16 tions necessary for the onset of multi-plate tectonics.

17 ugh conventional subduction-style horizontal tectonics.

18 y the topographic load, but not the regional tectonics.

19 subduction at that time and therefore plate tectonics.

20 ion and reflects the processes driving plate tectonics.

21 k-started the modern episode of active plate tectonics.

22 w the other, and the primary driver of plate tectonics.

23 Ma and potentially since the onset of plate tectonics.

24 nifested at the surface as present-day plate tectonics(1).

25 beneath this boundary is essential for plate tectonics, a consensus on its origin remains elusive.

26 duction is a typical feature of modern plate tectonics, a stagnant-lid tectonic regime with localized

27 e 'boring billion'-a period of reduced plate tectonic activity about 1.75 to 0.75 billion years ago t

28 s to the onset of renewed intensification of tectonic activity and mountain building, the development

29 Together, the renewed tectonic activity and oceanographic changes facilitated

30 ape brought about by previously unrecognized tectonic activity in the East African rift system.

31 Himalayan tectonic activity is triggered by downward penetration o

32 Coupled magmatic and tectonic activity plays an important role in high-temper

33 Plate tectonics affect geography, but also atmosphere composit

34 ients required deep lamellar keratoplasty (2 tectonic and 1 optical), and 2 underwent cornea gluing a

35 formed in 21 of 36 eyes (58%), 9 therapeutic/tectonic and 12 for visual rehabilitation.

36 ux of dissolved iron to seawater than active-tectonic and dysoxic continental margins.

37 t mantle heterogeneity and its links to past tectonic and geodynamic processes.

38 h this broad region has a relatively uniform tectonic and geologic history, the thermal regimes of it

39 s of 10(4)-10(7) years and is independent of tectonic and geomorphic setting.

40 ion, it can also reveal insights into former tectonic and geomorphological processes.

41 nt resulted from progressive focusing of the tectonic and magmatic activity into an oblique, throughg

42 Upon evaluating the overlap between tectonic and Milankovitch periodicities across spreading

43 hese results highlight the crucial impact of tectonic and oceanographic processes on mangrove OC sequ

44 r tectonic indications and risk factors for (tectonic and physiologic) graft failure.

45 pore water iron isotope data from a passive-tectonic and semi-arid ocean margin (South Africa), whic

46 Young rifts are shaped by combined tectonic and surface processes and climate, yet few reco

47 ancient material have eluded destruction by tectonic and surface processes operating over billions o

48 early Earth are currently explained by plate tectonic and vertical tectonic models, but these do not

49 As continental rift zones mature the tectonic and volcanic processes associated with crustal

50 ral Asian Orogeny Belt (CAOB) due to varying tectonic and weathering controls.

51 rth history, implying a lack of modern plate tectonics and a paucity of subaerial crust, and conseque

52 crobial isotope effects or abrupt changes to tectonics and associated pyrite burial.

53 of isolating the respective contributions of tectonics and climate to erosion.

54 h's surface archives the combined history of tectonics and erosion, which tend to roughen landscapes,

55 Pluto's large moon Charon displays tectonics and evidence for a heterogeneous crustal compo

56 alysing mantle convection, lubricating plate tectonics and feeding arc volcanism.

57 Geologic process, including tectonics and global climate change, profoundly impact t

58 Plate tectonics and mantle dynamics necessitate mantle recycli

59 This drives surface tectonics and pre-conditions the margins for further def

60 e adiabatic value and is suggestive of plate tectonics and/or advective magmatic heat transport.

61 ort bed sediment, independently of climatic, tectonic, and bedrock controls.

62 to improve models of past glacial, eustatic, tectonic, and geomorphic processes on continental shelve

63 d China and an assessment of the geomorphic, tectonic, and lithologic controls on quake-induced lands

64 al to our understanding of the physiography, tectonics, and climate of our planet at the dawn of life

65 opographic rings, dominate the stratigraphy, tectonics, and crustal structure of the Moon.

66 ents-is incompatible with modern-style plate tectonics, and favours instead the formation of TTGs nea

67 ediment supply in feedbacks between climate, tectonics, and mountain landscape evolution.

68 and quantifiable part in shaping topography, tectonics, and seismic hazard within intraplate settings

69 mbbell shapes and are prepared by a parallel tectonic approach under ambient conditions.

70 ction (about 4 billion years ago) and global tectonics (approximately 3 billion years ago) suggests t

71 ly processes in real time to build arbitrary tectonic architectures.

72 together with crust recycling through plate tectonics, are the primary processes that drive the chem

73 rocks, suggesting the onset of global plate tectonics at ~3.0 billion years ago.

74 his gateway, together with subsiding volcano-tectonic barriers would have played a key role in Late C

75 lts that shed light on the interplay between tectonics, basin migration and faunal change on the one

76 y different before the onset of global plate tectonics because most present-day subduction initiation

77 entific theories of how subduction and plate tectonics began on Earth--and what the tectonic structur

78 ies to the center, squeezed up by more rigid tectonic blocks in the north and south.

79 kilometres to form boundaries between rigid tectonic blocks.

80 odology, to pinpoint interaction between the tectonic building blocks that construct the metal-organi

81 t, corresponding to independently determined tectonic changes.

82 es quantitatively as a result of climatic or tectonic changes.

83 us landscapes is a complex interplay between tectonics, climate and denudation.

84 erstanding how environmental forcings (e.g., tectonics, climate) are transformed by erosional landsca

85 on of depositional systems that may preserve tectonic, climatic and anthropogenic signals.

86 ecent work indicates a large increase in the tectonic CO(2) degassing rate between the Neoproterozoic

87 ted damage and weak zones, promote increased tectonic complexity, such as oblique subduction, strike-

88 The relative influences of tectonics, continental weathering and seafloor weatherin

89 rong influence of climate in addition to the tectonic control, and we propose that the post Miocene C

90 y assumed to accurately record climatic- and tectonic-controlled mountain denudation and play an impo

91 The initiation mechanism of Earth's plate tectonic cooling system remains uncertain.

92 usly overlooked coupling between Phanerozoic tectonic cycles, the major-element composition of seawat

93 d rock uplift is important for understanding tectonic deformation in this region.

94 he Appalachian Structural Front, a proxy for tectonic deformation), distance to gas wells was highly

95 patterns are attributed to primary geology, tectonic deformation, followed by fluvial erosion (and l

96 by episodes of intense volcanic activity or tectonic deformation.

97 complex interplay of volcanic accretion and tectonic dismemberment of the oceanic crust, resulting i

98 ence only subduction zones survive and plate tectonics does not spread, which corresponds to observat

99 ncreased organic burial and that alternative tectonic drivers (erosion, outgassing) provide testable

100 , including the North Sea, implying a common tectonic driving force.

101 ng 500,000 seismograms (250k associated with tectonic earthquakes and 250k identified as noise) recor

102 age adjustment or other local (for example, tectonic) effects.

103 When plate tectonics emerged and how it has evolved through time ar

104 cs, as it gives insight into the geohistory, tectonic environment, geohazard mitigation, etc.

105 ing, exhumation and cooling that reflect the tectonic environments in which they formed(5,6).

106 , responsible for orocline formation and the tectonic escape of the back arc region, is imaged here f

107 ystem develops, as well as the mechanism for tectonic escape of the back-arc region.

108 sing the 2011 event reveals that this single tectonic event delivered >1 Tg of organic carbon to the

109 The hiatuses coincide with regional tectonic events and changes in global thermohaline circu

110 features are well correlated with historical tectonic events in this region, such as extension along

111 Here it is considered that the tectonic events that produced the natural cracks in shal

112 New constraints on the tectonic evolution of the Neo-Tethys Ocean indicate that

113 t of the Mid-Atlantic Ridge to constrain the tectonic evolution of these blocks.

114 s may force a reexamination of models of the tectonic evolution of western North America over the las

115 tal amalgamation-we further argue that plate tectonics exerted an overarching control on biodiversity

116 tion, such as tilts or dissection by renewed tectonic extension, depending on their positions with re

117 uctions may be superimposed on a first-order tectonic fabric, we emphasize the difficulty of decipher

118 Risk factors for tectonic failure (18/362 eyes, 5.0%) were severe lid dis

119 ock friction have elucidated many aspects of tectonic fault zone processes and earthquake phenomena.

120 -resolution studies of elastic properties in tectonic fault zones may aid in the search for reliable

121 Tectonic faults also fail in slow earthquakes with ruptu

122 ke is a result of interplay among injection, tectonic faults, and foreshocks.

123 rthquakes and slow-slip events, occurs along tectonic faults.

124 veloped diachronously and represent regional tectonic features rather than a synchronous global pheno

125 D seismic lines and bathymetric data, we map tectonic features such as faults, crustal highs, and ind

126 kely to have been largely regulated by plate tectonics for most of its history.

127 chemical change that reveal shifts in global tectonic forces connecting Earth ocean-climate processes

128 icate weathering that regulates climatic and tectonic forcing through hydrologic processes and impose

129 red rates of vertical displacement caused by tectonic forcing, and their relationships are consistent

130 s is controlled by the erosional response to tectonic forcing.

131 t of the Sturtian glaciation has suggested a tectonic forcing.

132 sing tomographic data, we recreate the plate-tectonic geometry of the subducted Nazca slab, which ena

133 mangroves are controlled by the interplay of tectonics, global sea level and sedimentation, including

134 as significantly better than therapeutic and tectonic grafts at all time points.

135 r anatomically successful cases with central tectonic grafts, active corneal inflammation and donor s

136 in anatomically successful eyes with central tectonic grafts.

137 (1,7,8)) or that suggested that modern plate tectonics has operated since the Palaeoproterozoic era (

138 diversification, to document how climate and tectonics have driven ecosystem and evolutionary dynamic

139 tonics of the region, pose both volcanic and tectonic hazards to the city of Rome, located 20 km to t

140 ked to the variation of regional climate and tectonic history.

141 ognition of this plume force has substantial tectonic implications: the speed-up and slowdown of Indi

142 that cannot be completely explained by plate tectonic-imposed vicariance.

143 Subduction tectonics imposes an important role in the evolution of

144 sion central to the interplay of climate and tectonics in landscape evolution.

145 evious arguments for the importance of plate tectonics in the Cambrian radiation, namely the breakup

146 The operation of plate tectonics, in general, depends intimately on the manner

147 Outcomes of corneal transplantation for tectonic indications and risk factors for (tectonic and

148 Feedbacks between climate, erosion and tectonics influence the rates of chemical weathering rea

149 ution, the ocean-atmosphere system and plate tectonics is a central goal of Earth science.

150 Plate tectonics is among the most important geological process

151 ution of the planetary interior during plate tectonics is controlled by slow convection within the ma

152 narios for the onset of subduction and plate tectonics is hampered by the fact that subduction initia

153 A primary consequence of plate tectonics is that basaltic oceanic crust subducts with l

154 heric plates and basaltic magmatism of plate tectonics, is a key unknown in the evolutionary history

155 The megathrust north of the Median Tectonic Line is interseismically locked, has a history

156 ents the offshore continuation of the Median Tectonic Line, which onshore juxtaposes geological terra

157 t global data and to the variable effects of tectonics, lithology, land surface properties and human

158 mantle and play an important role in global tectonics, magmatism and volatile cycle.

159 osed feedbacks among topography, climate and tectonics may occur.

160 from clustered-Fe domains and 1,412+/-56 Ma (tectonic metamorphism) from planar and subgrain boundary

161 pressure differences cannot be explained by tectonic mixing, retrogression of high-pressure minerals

162 Most tectonic models have assumed that the subducting oceanic

163 tly explained by plate tectonic and vertical tectonic models, but these do not offer a global synthes

164 on spicules with skeletonlike morphology, 3D tectonic motifs, and reduced symmetries.

165 roach(7) that is designed to isolate secular tectonic motions from the daily GNSS time series to show

166 ism are typical surface expressions of plate tectonic movement on top of narrow plumes of hot materia

167 We argue that tectonic movements were the primary control on the clima

168 agnetic field, convective mantle, mobile lid tectonics, oceans of liquid water, dynamic climate and a

169 (MSVD), Italy, coupled with the extensional tectonics of the region, pose both volcanic and tectonic

170 d to explain the complex oceanic-continental tectonics of these subduction zones.

171 The initiation of plate tectonics on Earth is a critical event in our planet's h

172 creation of short-wavelength relief by plate tectonics on Earth.

173 has been crucial in the development of plate tectonics on Earth.

174 n the Southern Ocean that was enabled by the tectonic opening of key oceanic gateways during the brea

175 from greenhouse to icehouse climates to the tectonic opening of Southern Ocean gateways, more recent

176 rement interval complicates efforts to infer tectonic or climatic forcing from changes in rates of ri

177 les, while local, basin-scale changes (e.g., tectonic or hydrographic) and biotic interactions ruled

178 ies as a function of strain accommodation by tectonic or magmatic processes.

179 thern Sierra Nevada previously attributed to tectonic or mantle-derived forces is partly a consequenc

180 ers are created by external factors, such as tectonics, or base-level change.

181 Ideas leading to the hypothesis of plate tectonics originated largely with an oceanic focus, wher

182 been common since the onset of modern plate tectonics, our findings suggest that similar processes m

183 The Andean margin is the plate-tectonic paradigm for long-lived, continuous subduction,

184 on-deformation relationship is influenced by tectonic, petrological and volcanic factors.

185 e been traditionally explained by successive tectonic phases of 2-dimensional deformation.

186 rofiles across the asthenosphere for various tectonic plate ages.

187 Earthquakes far from tectonic plate boundaries generally exploit ancient faul

188 Although the surface deformation of tectonic plate boundaries is well determined by geologic

189 urface that show no obvious association with tectonic plate boundaries.

190 us convection within the mantle is linked to tectonic plate motions and deforms Earth's surface acros

191 in which the lithosphere comprised a single tectonic plate, with only the warmer, lower crust involv

192 Tectonic plates are a key feature of Earth's structure,

193 te boundaries and eventually to fully formed tectonic plates driven by subduction alone.

194 thenospheric layer underlying Earth's mobile tectonic plates is fundamental to our understanding of m

195 Because the inertia of tectonic plates is negligible, plate velocities result f

196 The majority are believed to form as Earth's tectonic plates move over long-lived mantle plumes: buoy

197 Tectonic plates that fragment ancestral ranges (vicarian

198 lling due to viscous drag from the diverging tectonic plates, but have been challenged by geophysical

199 l (2D) fragments, from mud cracks to Earth's tectonic plates, has two attractors: "Platonic" quadrang

200 rrestrial systems, we demonstrate that plate tectonics played a major role in driving tropical marine

201 w subduction zones initiate is a fundamental tectonic problem, yet there are few well-constrained geo

202 it is the result of the large compressional tectonic process.

203 discoveries allow us to understand regional tectonic processes and highlight the importance of satel

204 ks between tropical reef availability, plate tectonic processes and marine biodiversity distribution

205 Normal plate tectonic processes are responsible both for plate bounda

206 eformation within mountain ranges relates to tectonic processes at depth is not well understood.

207 ond inclusions is consistent with changes in tectonic processes that formed the continental lithosphe

208 time of global climatic changes and ongoing tectonic processes that formed the East African Rift.

209 The degree to which short-term non-tectonic processes, either natural and anthropogenic, in

210 that are not directly associated with plate tectonic processes.

211 cured or destroyed by surface weathering and tectonic processes.

212 ore reflect the secular evolution of Earth's tectonic processes.

213 recycling of seawater-derived neon in plate tectonic processes.

214 -type mantle has reached the southern tip of tectonic propagation in the southern Lau basin.

215 e morphology may be used to infer changes in tectonic rates.

216 crustal perspective must balance slow (plate tectonic) rates of melt generation and segregation in th

217 Here we infer from a tectonic reconstruction of the Andes constructed in a ma

218 ls embedded with the latest geological paleo-tectonic reconstructions and ground-truthed with new Hf-

219 and quadrupole moments of plate motions from tectonic reconstructions extended back to the early Meso

220 The timing is consistent with recent tectonic reconstructions of a relatively narrow Central

221 e global length of subduction zones in plate tectonic reconstructions, and by sea-level inversion.

222 ng to show that this can be explained by the tectonic recycling of previously accumulated sedimentary

223 Here we show that Earth's modern plate tectonic regime has developed gradually with secular coo

224 re of modern plate tectonics, a stagnant-lid tectonic regime with localized episodic subduction likel

225 ial of early Martian crust in a stagnant-lid tectonic regime, in which the lithosphere comprised a si

226 Valentine and Moores hypothesized that plate tectonics regulates global biodiversity by changing the

227 provide new insight into strike-slip volcano-tectonic relations by analysing Bouguer gravity data fro

228 lab into the lower mantle; the role of plate tectonics remains unclear, owing to the extensive subduc

229 Plate tectonics requires the formation of plate boundaries.

230 Its causes remain unresolved, with tectonic restrictions to the Atlantic Ocean or glacio-eu

231 nderstood more than 40 years after the plate tectonic revolution.

232 Biological or tectonic revolutions have been proposed to explain each

233 a combination of multiple forcings, such as tectonics, sea-level fall and long-term decline in green

234 mental controls on magma metal fertility are tectonic setting, the nature of source rocks, and magma

235 hich display geometries commonly observed in tectonic settings affected by interacting plate boundari

236 -constrained geologic tests that address the tectonic settings and dynamics of the process.

237 ence the occurrence of earthquakes in active tectonic settings or 'stable' plate interiors, remains a

238 centrations of magmas formed in a variety of tectonic settings using in situ trace-element measuremen

239 based on observations compiled from various tectonic settings(6-8) have suggested that the moment of

240 In both tectonic settings, our results indicate that fractional

241 evolution of the Earth's crust in a range of tectonic settings.

242 ent continental lithosphere in certain plate tectonic settings.

243 measured uplift is potentially attributed to tectonic shortening, lithospheric delamination and unloa

244 Further quantification of tissue tectonics showed patterns of rotations, contractions and

245 which enables us to reconstruct Andean plate tectonics since the late Mesozoic.

246 oving northwestward 11 mm a(-1) as part of a tectonic sliver.

247 he Mesozoic and later, long-lasting relative tectonic stability.

248 se is important for understanding when plate tectonics started and how the supply of nutrients to the

249 jor implication is that much of the prograde tectonic strain is accommodated by frictional slip on ma

250 advantages of this procedure include greater tectonic strength and less dry eye.

251 displaced in the direction of the prevailing tectonic stress (prograde), a large number of them are d

252 ntial portion of the spreading may be due to tectonic stress building up to a critical level rather t

253 as well as key complexities of the regional tectonic stress field.

254 least 35 kilometres of the ridge axis, where tectonic stress had built up to a critical level, trigge

255 The roles of magma pressure and tectonic stress in the development of seafloor spreading

256 Tarim Basin rather than in the compressional tectonic stress regime as in the periphery of the Tarim

257 , nearby fault that is experiencing regional tectonic stress.

258 e much smaller than the magnitude of ambient tectonic stresses in the crust at depth.

259 tions predict these results, suggesting that tectonic stresses interact with topography to influence

260 hy where the ratio of horizontal compressive tectonic stresses to near-surface gravitational stresses

261 emperature-dependent rheologies and external tectonic stresses.

262 Here we show the first evidence of a major tectonic structure in its initial-stage, the Al-Idrissi

263 plate tectonics began on Earth--and what the tectonic structure of Earth was before this--remain enig

264 The spatial pattern of magmatic-tectonic structures bounding Procellarum is consistent w

265 ravity models are powerful tools for mapping tectonic structures, especially in the deep ocean basins

266 features not previously resolved, including tectonic structures, volcanic landforms, basin rings, cr

267 tudies that inferred an abrupt transition in tectonic style in the Neoproterozoic era (about 0.7 bill

268 ove organic carbon (OC) was promoted by high tectonic subsidence and fluvial sediment supply.

269 obtained in this way, after corrections for tectonic subsidence, yield cyclic relative sea-level (RS

270 Plate tectonics successfully describes the surface of Earth as

271 s are some of the weakest parts of the plate tectonic system, but previous studies have not favored t

272 sphere is one of the central themes of plate tectonics, the recycling of continental lithosphere appe

273 uch as the separation of continents by plate tectonics, the uplift of mountains or the formation of l

274 challenging, as it requires extending plate tectonic theory to the dynamics of continental deformati

275 stress-loading is dominated by the regional tectonics through slip on underlying shear zones and fau

276 mixing and thus a potential tracer of plate tectonics through time.

277 For plate tectonics to operate on a terrestrial planet, the surfac

278 e we extrapolate models of present-day plate tectonics to the past and propose that since about three

279 s from mantle flow beneath, and allows plate tectonics to work.

280 In the coherent Monte Rosa tectonic unit, Western Alps, considerably different meta

281 Fast axes are uniform within tectonic units and parallel to SKS axes, orogenic strike

282 al history of sedimentary basins, as well as tectonic uplift and denudation rates.

283 Our study does not disprove coupling between tectonic uplift and erosion but suggests that this coupl

284 ss balance is also significantly affected by tectonic uplift and erosion via changes to the inorganic

285 in the Neogene, is generally associated with tectonic uplift during collision of the Panama volcanic

286 California, United States, to assess whether tectonic uplift history can be reconstructed using measu

287 than today at 125 ka indicating net maximum tectonic uplift of 19 m with an average rate of 0.015 cm

288 ated erosion that migrates upstream (such as tectonic uplift or sea level change).

289 They communicate changes in sea level or tectonic uplift throughout landscapes(2,4) or stall rive

290 thering, this source is probably enhanced by tectonic uplift, and so may have contributed to the rela

291 or diffusive soil creep, runoff erosion, and tectonic uplift, is reminiscent of the subsequent instab

292 eathering that are consistent with increased tectonic uplift, more rapid continental denudation, incr

293 hism (as a proxy for secular change in plate tectonics) using a statistical evaluation of the distrib

294 and slow cooling, which gives rise to plate tectonics, volcanoes and mountain building.

295 growing consensus suggests that multi-plate tectonics was preceded by cooling through a single-plate

296 adrapur topographic high record an incipient tectonic wedge or triangle zone.

297 vide a modern snapshot of the development of tectonic wedges and lateral discontinuities preserved in

298 nvection provides the mechanism behind plate tectonics, which allows oceanic lithosphere to be subduc

299 e, however, an update of the theory of plate tectonics would be expected with continuing discovery of

300 key role in terrestrial magmatism and plate tectonics, yet despite experimental demonstration of the