乌克兰南极站地区(西南极洲威廉群岛)首次发现圆形长石

IF 0.5 Q4 MINERALOGY Mineralogical Journal-Ukraine Pub Date : 2021-01-01 DOI:10.15407/mineraljournal.43.02.040
O. Mytrokhyn, V. Bakhmutov
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引用次数: 0

摘要

作者在南极洲西部发现了一种新的圆形结构火成岩。发现地点是位于南极半岛格雷厄姆海岸附近的威廉群岛的Hovgaard岛。直到现在,在这个地区还没有发现这些稀有岩石的踪迹。通常圆形岩石是在多种地质成岩因素局部“重合”的条件下形成的。对Hovgaard岛圆形岩石的地质位置、结构特征和矿物组成进行了研究,以建立其初步的岩石学描述。结果表明,在角闪辉长岩及其侵入角砾岩中,出露圆形长砾岩面积较小,约为200 m2。圆形石的产状和结构表明它们的结晶发生在浅成岩深度。该产状可能是一个小型辉长岩侵入体的边缘相,部分辉长岩侵入体暴露在Hovgaard岛邻近的沿海地区。研究表明,Hovgaard岛的圆长岩属于这些岩石中最稀有的岩石学代表,即圆形辉长岩。在岩石学特征上,它们与暴露在科西嘉岛上的著名的法国拿破仑岩(尸体)有明显的不同。其矿物组成主要为钙斜长石(An88-97)、角闪石(#Mg = 0.77-0.81)、斜辉石(wo48 - 50en43 - 47f5 -8)、尖晶石(Sp62-72Hrc14-20Mt12-17)、放光石、绿泥石、磁铁矿和磷灰石。圆间基质具有辉长石组成和斑状织构。它与圆石的不同之处在于钙斜长石较少,镁角闪石较少,而且没有尖晶石。鉴于圆形辉长岩的罕见性和所描述的表现形式的特殊性,建议将Hovgaard岛的圆形辉长岩视为辉长岩科的一个新的岩石学变种。推荐将这种圆形辉长岩命名为“hovgaardite”。
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First Finding of the Orbicular Gabbroids in the Ukrainian Antarctic Station Area (Wilhelm Archipelago, West Antarctica)
A new occurrence of igneous rocks with an orbicular structure was discovered by the authors in West Antarctica. The place of finding is Hovgaard Island in the Wilhelm Archipelago located near the Graham Coast of the Antarctic Peninsula. Until now, not a single manifestation of these rare rocks was known in this region. Usually orbicular rocks are formed under the condition of local "coincidence" of many geological and petrogenetic factors. The study of the geological position, texture features and mineral composition of the orbicular rocks on Hovgaard Island was carried out in order to create their primary petrographic description. It was found that orbiculites are exposed in a small area, about 200 m2, in the field of amphibolized gabbroids and their intrusive breccias. The occurrence and textures of the orbiculites indicate that their crystallization occurred at the hypabyssal depth. Probably, this occurrence is a marginal facies of a small gabbroid intrusion, some parts of which are exposed on the adjacent coastal areas of Hovgaard Island. The studies performed have shown that the orbiculites of Hovgaard Island belong to the rarest petrographic representatives of these rocks namely orbicular gabbroids. In their petrographic feature, they differ markedly from the famous French napoleonites (corsites) exposed on the Corsica Island. The mineral composition of the orbicules is represented by calcium plagioclase (An88-97), hornblende (#Mg = 0.77-0.81), clinopyroxene (Wo48-50En43-47Fs5-8), spinel (Sp62-72Hrc14-20Mt12-17), actinolite, phlogopite, chlorite, magnetite and apatite. The interorbicular matrix has a gabbroid composition and a porphyritic texture. It differs from orbicules in somewhat less calcium plagioclase and less magnesian hornblende, as well as in the absence of spinel. In view of the rarity of orbicular gabbroids and the specificity of the described manifestation, it is proposed that the orbicular gabbro on Hovgaard Island be considered as a new petrographic variety of the gabbroid family. The name "hovgaardite" is recommended for the name of this variety of orbicular gabbro.
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