Results 171 to 180 of about 24,652 (211)
Inefficient melt mixing below a fast-spreading ridge revealed by Hess Deep lower gabbros (ODP Leg 147 and IODP Expedition 345). [PDF]
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2023
—after Privilege and Romanticism in adjacent droughts they laze the fields like heifers with attentive palms out for borrowed cud / spread eagle or prim / demure afloat in ponds, among the fronds, dainty jowls nestled in knightly palms / those wild, windrow
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—after Privilege and Romanticism in adjacent droughts they laze the fields like heifers with attentive palms out for borrowed cud / spread eagle or prim / demure afloat in ponds, among the fronds, dainty jowls nestled in knightly palms / those wild, windrow
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Russian Geology and Geophysics, 2008
Abstract Epidote is traditionally considered a mineral indicating metamorphic and metasomatic genesis of rocks. Recently, the magmatic nature of epidote of many granitoid intrusions has been proved. We present the first data on the magmatic origin of epidote, which is one of the rock-forming minerals of anorthite fassaite and biotite ...
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Abstract Epidote is traditionally considered a mineral indicating metamorphic and metasomatic genesis of rocks. Recently, the magmatic nature of epidote of many granitoid intrusions has been proved. We present the first data on the magmatic origin of epidote, which is one of the rock-forming minerals of anorthite fassaite and biotite ...
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2011
The geology of the East Sooke peninsula comprises a core of olivine gabbro, peripherally uralitized and bounded on the north and east by upper Eocene Metchosin basalts of submarine origin. The gabbro intrudes the basalts which are unconformably overlain by sediments of the Sooke Formation of Miocene-Oligocene age.
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The geology of the East Sooke peninsula comprises a core of olivine gabbro, peripherally uralitized and bounded on the north and east by upper Eocene Metchosin basalts of submarine origin. The gabbro intrudes the basalts which are unconformably overlain by sediments of the Sooke Formation of Miocene-Oligocene age.
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Science in China Series B, 2003
We call a subgroup H of a finite group G c-supplemented in G if there exists a subgroup K of G such that G = HK and H ∩ K ≤ core(H). In this paper it is proved that a finite group G is p-nilpotent if G is S 4-free and every minimal subgroup of P ∩ G N is c-supplemented in N G(P), and when p = 2 P is ...
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We call a subgroup H of a finite group G c-supplemented in G if there exists a subgroup K of G such that G = HK and H ∩ K ≤ core(H). In this paper it is proved that a finite group G is p-nilpotent if G is S 4-free and every minimal subgroup of P ∩ G N is c-supplemented in N G(P), and when p = 2 P is ...
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Differentiated Gabbro Intrusives
2001The extrusion of large volumes of tholeiite basalt on the continents discussed in Chap. 5 has been an important phenomenon throughout most of geologic time. Remnants of Precambrian basalt plateaus still exist in scattered locations on the Precambrian shields of the major continents (e.g.
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