Is anorthosite intrusive or extrusive

Translation of "intrusive rocks" in German

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YRM-10-RC055 intersected similarly silicified and pyritized intrusive rocks from 16 to 22 meters.
YRM-10-RC055 intersected a similar silicified and pyritized Intrusive rock between 16 to 22 meters.
The company has completed 4 drill holes which show visible mineralization in the structures, mantos and intrusive rocks.
The company has completed 4 drill holes showing significant mineralization in the structures, manto deposits and intrusive rocks point out.
This zone of intrusive rocks has also demonstrated increased magnetic intensity.
Trenching in the central area indicates it is underlain by intrusive rocks with potassic and propylitic alteration similar to the North, South and Tizate zones.
The excavations in the center of the area indicate that this is from Intrusive rock with potash and propylitic alteration similar to that of the North, South and Tizate Zones.
The zone is hosted by granodiorite intrusive rocks and is not exposed on the easternmost end where it is overlain by younger volcanic rocks and colluvial sediments.
The zone lies in granodiorites intrusive rocks and does not show up at the easternmost end where it is overlaid by younger volcanic rocks and colluvial sediments.
YRM-10-RC036 encountering intensely silicified and pyritized intrusive rocks below the surface anomaly and the hole was lost at a depth of 90 meters.
YRM-10-RC036 penetrated an intensely silicified and pyritized one Intrusive rock below the surface anomaly and the hole was lost at a depth of 90 meters.
The project is located within the southernmost portion of the Chihuahua Trough, where alkaline dikes and sills along the caldera ring fracture of the Trough carry semi-massive sulphide stockwork zones in altered intrusive rocks.
The project is located in the southernmost portion of the Chihuahua Trough, where alkaline storage and traverses along the caldera ring fault of the trough have altered semi-massive sulphide bedding zones Intrusive rock accommodate.
The intrusive rocks belonging to this family are called granite or granodiorite, depending on whether, respectively, are rich or poor in quartz. Among the effusive rocks of this family, however, it is important to remember the rhyolite (corresponding effusive granite).
The intrusive rocks From this family are granite or granodiorite, depending on whether, or, rich or poor in quartz. However, among the effusive rocks of this family, it is important to remember the rhyolite (appropriately effusive granite).
This newly acquired 40 claim (1,000 hectare) license is underlain by mafic intrusive rocks including gabbro, norite and anorthosite.
The bedrock of the newly acquired concession area with the 40 claims (1,000 hectares) is being used by a mafic Intrusion complex formed from gabbro, norite and anorthosite.
Ore geology at the Seabee Gold Operation consists of high-grade vein mineralization associated with shear zones that transect mafic meta-volcanic and intrusive rocks, as well as granitic rocks emplaced during the regional deformation events impacting the Pine Lake greenstone belt during the Proterozoic.
The geology at the Seabee gold operation consists of high grade vein mineralization associated with shear zones, the mafic metavolcanic and Intrusive rocks cuts through as well as granite rock stored during the regional fault events that affected the Pine Lake greenstone belt in the Proterozoic.
One area surrounds the gossan zone and measures approximately 500 x 150 meters in size, and is potentially open along strike. The other gold anomaly is related to beds of an altered calcareous sandstone unit that lies in close proximity to altered intrusive rocks.
One area surrounds the Iron Hat Zone and is approximately 500m by 150m; this area may be open along strike; the other gold anomaly is associated with an altered calcareous sandstone formation in close proximity to altered Intrusive rock is located.
The intrusive rocks consist mainly of coarse grained granite and medium sized grained diorite. Within the diorite sometime rock floes of gabbro can be found. Pegmatitic and aplitic transitional rocks are common.
The Intrusive rocks consist mainly of coarse-grained granite and medium-grained diorite. Occasionally, gabbro plugs appear within the diorite. Pegmatitic and aplitic gaits are common.
Miranda proposes that the Iron Point alteration and gold anomalies with their associated west-northwest and northwest-trending dike patterns may occur within a broad zone of intrusive rocks and interrelated faults and folds extending west-northwest from the Lone Tree Mine area.
Miranda suspects that the alteration and gold anomalies at Iron Point and the associated west-northwest and northwest-trending earthworks are within a broader zone intrusive rock and intervening fractures and folds that extend west-northwest of the Lone Tree Mine area.
Sample composites consisting of mixed metamorphic and intrusive rocks representative of the mineralized zones were prepared by SGS from 188 kilograms of drill sample rejects. SGS prepared two variability samples from these composites with each sample being blended, crushed, split and combined into one sub-composite.
The samples consist of mixed metamorphic and intrusive rock and are representative of the mineralized zones. The samples prepared by SGS came from 188 kg prepared 2 variable samples from these composites, each sample being blended, ground, split and combined into a sub-sample.
The Millesvaches Massif is also oriented North-South and consists like the Saint-Mathieu dome largely of intrusive rocks rimmed by micaschists of the PMU.
The Millesvaches massif, which is also north-south, consists, like the Saint-Mathieu-Dom, for the most part Intrusive rocks and is largely framed by mica schists of the parautochthonous mica schist unit.
The source of ore within manto deposits is considered to be interformational, from a sedimentary source within an adjacent sedimentary basin, or from ore fluids driven off from intrusive rocks.
The ore in a Manto deposit comes from other formations or is from sediments from an adjacent sedimentation basin or from ore-containing fluids from Intrusive rock originated.
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