コーパス検索結果 (１語後でソート)
通し番号をクリックするとPubMedの該当ページを表示します
1 an isotopic signature indistinguishable from mid-ocean ridge basalt.
2 the highest values previously measured in a mid-ocean-ridge basalt.
3 ction of melt and recycling of the resulting mid-ocean-ridge basalt.
4 sulphur and chlorine in the source of normal mid-ocean-ridge basalt.
5 rc magmas are indistinguishable from that of mid-ocean ridge basalts.
6 riking chemical and isotopic similarities to mid-ocean-ridge basalts.
7 ve helium concentrations of ocean island and mid-ocean-ridge basalts.
8 es to rise to become the source material for mid-ocean-ridge basalts.
9 peridotite can indeed be the sole source for mid-ocean-ridge basalts.
10 nents as sampled by ocean island basalts and mid-ocean-ridge basalts.
11 ts are very similar to primitive terrestrial mid-ocean ridge basalts and indicate that some parts of
12 r mantle, produce the isotopic signatures of mid-ocean ridge basalts and oceanic island basalts, and
13 he differences in (3)He/(4)He ratios between mid-ocean-ridge basalts and ocean island basalts, as wel
15 mantle, beneath the upper mantle sampled by mid-ocean-ridge basalts, and that buoyantly upwelling pl
16 stinct chemical signatures, ocean-island and mid-ocean-ridge basalts are traditionally inferred to ar
17 th the dominant 4He/3He peak found in modern mid-ocean-ridge basalts, as well as estimates of the ini
18 d basalts (OIBs) have lower Re contents than mid-ocean ridge basalt, because garnet-bearing residues
19 , ocean ridge depths, and the composition of mid-ocean ridge basalts can all be used to determine var
21 s (NMORBs) and incompatible element-enriched mid-ocean ridge basalts (EMORBs) as far as 20 kilometers
23 pre-eruptive volatile content for a suite of mid-ocean-ridge basalts from the Siqueiros intra-transfo
25 e origin of the isotopic signature of Indian mid-ocean ridge basalts has remained enigmatic, because
27 , presumably because the volatile content of mid-ocean-ridge basalts is generally too low to produce
28 In contrast, the upper mantle, as sampled by mid-ocean ridge basalts, is highly depleted in incompati
29 made for degassed and chlorine-contaminated mid-ocean-ridge basalt magmas, and hence constrain degas
37 in ocean island basalts (OIBs) compared with mid-ocean-ridge basalts (MORBs) have been used as eviden
38 with lower and relatively uniform values in mid-ocean-ridge basalts (MORBs), are thought to result f
40 ndicate near-symmetrical eruptions of normal mid-ocean ridge basalts (NMORBs) and incompatible elemen
41 the incompatible element-depleted source of mid-ocean ridge basalts, possibly as a result of a globa
42 We report 230Th-238U disequilibrium data on mid-ocean ridge basalts recovered 5 to 40 kilometers off
43 nough to affect major portions of the Indian mid-ocean ridge basalt source region has been a long-sta
47 mitive arc magmas have identical Zn/Fe(T) to mid-ocean-ridge basalts, suggesting that primary mantle
48 o the lower (3)He/(4)He ratios identified in mid-ocean-ridge basalts that form by melting the upper m
50 and) basalts seem to contain more water than mid-ocean-ridge basalts, we demonstrate that basalts ass
51 5 per cent relative to 226Ra occur in normal mid-ocean ridge basalts, with the largest deficits in th
WebLSDに未収録の専門用語（用法）は "新規対訳" から投稿できます。