ライフサイエンスコーパス: granite

1 ith an age of >=676 +/- 26 Ma cut Pikes Peak granite.

2 ux and slip style in shear experiments along granite and diorite laboratory faults, during which the

3 ne directly overlies Tavakaiv-injected Pikes granite and drapes over core stones in Pikes regolith, c

4 ties varied as a function of rock type, with granite and limestone tombstones from the same cemeterie

5 The granite and limestone-associated communities also had di

6 ng incipient weathering of basalt, rhyolite, granite and schist depends on the activity of microbes,

7 ogy to zircon from the Quaternary Kurobegawa Granite and Takidani Granodiorite in the Hida Mountain R

8 Typically found in rare-metal granites and pegmatites, lithium micas are increasingly

9 Basalt, granite, and quartz (53-250 um) were deployed in surface

10 the production of anorthosites and Rapakivi granites, and giving rise to extreme thermobaric ratios

11 if-type anorthosites and anorogenic Rapakivi granites are largely confined to this period and the tem

12 Granites are nearly absent in the Solar System outside o

13 lso had distinct functional attributes, with granite-associated bacteria having more genes linked to

14 residence within, and assimilation of, local granite basement.

15 e juxtaposes geological terranes composed of granite batholiths (in the north) and accretionary compl

16 olatile compounds of Verdelho wines from the Granite Belt have been isolated by solid phase extractio

17 o is a white-grape-vine, growing well in the Granite Belt region of Queensland.

18 l faults, which were made of room-dry, solid granite blocks, quickly wore to form a fine-grain rock p

19 hering crusts inherited REE signature of the granites, but show more Ce depletion and more overall co

20 radionuclide disposal is mostly conducted in granite, clay, saltstone, or volcanic tuff formations.

21 As the granites crystallised, late stage melts were intruded th

22 gent of crustal differentiation, but linking granite emplacement to crust formation requires knowledg

23 son et al. proposed that plate tectonics and granites existed 4.5 billion years ago (Ga), within 70 m

24 heatre-headed gorge formation in unweathered granite from the overtopping of a rock-cut dam spillway

25 currence of unidentified REE minerals in the granites from South Chinese deposits.

26 Here, we show that granites from the eastern Peninsular Ranges Batholith (P

27 Granite generation ceased once enriched partial melts co

28 ss rich in silica and other light elements ("granite glass") had more "corrosion related" peaks than

29 t TTG magmatism may have taken place beneath granite-greenstone complexes developing along Archaean i

30 de metamorphic ('grey gneiss') and low-grade granite-greenstone terranes are comprised dominantly of

31 f similar age; and a glacial clast of A-type granite has a uraniun-lead zircon age of approximately 1

32 and seven natural mineral particles (basalt, granite, hematite, magnetite, mica, milky quartz, and cl

33 morphic aureole, and apply it to the Skiddaw granite in northern England.

34 These tracers indicate the presence of granites in East Antarctica having the same age, geochem

35 , and isotopic signatures as the distinctive granites in Laurentia.

36 minantly mined from the weathering crusts of granites in South China.

37 nsistent with evolved rocks similar to lunar granites in the Apollo samples.

38 The mechanism, temperature, and timescale of granite intrusion remain controversial, with wide-rangin

39 sampled at depth from an active system (Toki Granite, Japan), we show that, contrary to commonly prop

40 d layer overlying a low-permeability crushed granite layer containing a NAPL mixture of indane and be

41 ncreasing significantly in sequence: quartz, granite < basalt, olivine, limestone < gabbro.

42 that--far from being geologically sluggish--granite magmatism is a rapid, dynamic process operating

43 he town of Obertraun, Austria, surrounded by granite massifs.

44 wells were completed in bedrock composed of granite, metamorphic, and mafic rocks.

45 nnels inside weathered feldspars of the Shap granite (northwest England) has revealed modern bacteria

46 from the classic hornblende-bearing (I-type) granites of eastern Australia.

47 n detrital zircons match those in Laurentian granites of similar age; and a glacial clast of A-type g

48 linear dependence of the seismic velocity in granite on temperature and the associated acoustic emiss

49 on of silicic magmas leads to emplacement of granite plutons, huge explosive volcanic eruptions and p

50 ation of major elements during weathering of granite, rhyolite, schist and basalt was rock-specific a

51 hwestern domain, as well as along the Tichka granite's margin.

52 these drivers are absent on the Moon, small granite samples have been found, but details of their or

53 molecular products produced on heterogeneous granite samples with minimal sample preparation.

54 ements allow us to rapidly map an unpolished granite specimen (~ 2 x 2 mm) with an exceptionally high

55 Peanut protein was completely removed from granite tables after cleaning with detergent, and levels

56 rentiation alone may not be able to generate granites, the most silicic endmember making up the upper

57 This granite type forms by the reworking of sedimentary mater

58 asting crystalline rock system (Carnmenellis Granite, UK) corroborate these results.

59 during rupture and slip of initially intact granite under upper crustal conditions.

60 These observations provide evidence that the granite was exhumed and resided at the surface prior to

61 The origin of granites was once a question solely for petrologists and

62 from soils dominated by andesite, basalt or granite weathering and identified 3 families with high i

63 opically depleted sources, metasomatized the granites, which resulted in Ce depletion as Ce(4+) and e