ライフサイエンスコーパス: granite

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

2 The granite and limestone-associated communities also had di

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

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

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

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

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

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

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

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

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

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

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

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

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

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

17 Granite generation ceased once enriched partial melts co

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

38 This granite type forms by the reworking of sedimentary mater

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

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

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