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您的检索式：作者名="H.W.GreenII"
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| 1 | 台湾海峡上地幔流变学状态及其构造意义显示文摘本文详细研究了台湾澎湖列岛上地幔幔源包体的变形结构、组构和橄榄石位错构造。根据包体矿物(辉石)化学成分的计算,平衡温度为986—1116℃,压力为1.50—2.60GPa。上地幔变形事件可分为3个序列:(1)高温低应力均匀稳态流动变形;(2)高温较高应力上地幔底辟边缘的剪切流动变形;(3)低温高应变速率、{110}滑移条带的淬取变形。本区上地幔变形事件和热结构特征表明,福建东部和台湾澎湖列岛一带具有十分相似的上地幔流变学特征。澎湖列岛玄武岩的火山作用与台湾海峡上地幔热点有关,上地幔底辟作用和上涌是导致中国大陆边缘构造裂谷作用的主要原因。 | 金振民 金淑燕 H.W.GreenII 马长玲 | 1995 | 地质学报1995，69，1： | 8 |
| 2 | Mantle-derived Xenoliths and the Token of a Modern Back-Arc Geotherm Beneath Eastern China显示文摘Xenoliths of garnet and spinel-garnet 1herzolite from Mingxi, Eastern China have been studied in terms of comprehensive methods of mineralogy, petrology, fabrics, mierostructures and infrared spectrum. The temperature and pressure equilibration of the xenolith have been calculated using the TEMPEST program with the two-pyroxene geothermometer of Bertrand and Mercier (1985) combined with the geobarometer of Nickel and Green (1985). The temperature and pressure of xenoliths range from^1300 K at 1. 9 GPa (60 km) to ~1500 K at 2. 6 GPa (80 km). The geotherm inferred from xenolith is excellently consistent with the measured surface heat flow (70 mW/m2) in Mingxi. A character of geothermal curve and conductive type suggest that these xenoliths are from the lithosphere, not from the asthenosphere. The geotherm and mierostructures and preferred orientations of minerals in the xenolith are consistent with tecon-ic thinning of the lithosphere in the present-day extensional back-arc environment. | 金振民 H.W.GreenII R.S.Borch 金淑燕 T.N.Tingle T.E.Young | 1994 | Science China Chemistry1994，37，4： | 1 |
| 3 | 深源地震机制显示文摘大多数地震因脆性破裂和原有断层摩擦滑动发生在地表下数十公里范围内。然而,约占总数20%的地震发生在很大的深处(达680km),那里的高压制止了常规的断层活动。在高压下岩石会流动,而不会破裂,因而似乎不可能发生深震。在20年代发现深源地震之后,很快就认识到这种矛盾,此后一直未解决。 | H.W.GreenII 沈晶 | 1994 | 地震地质译丛1994，16，2： | 0 |
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