trondhjemite ['trɔnje,mait]
- trondhjemite的基本解释
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奥长花岗岩
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Occurs to the eastern Houshiding overturned anticline of Fuping complex domal uplift, Pingyang gneissic granite, a trondhjemite looks like a domal anticline in the west part and becomes two sub-anticlines overturned to south in the east part.
岩体的西部似一穹状背斜,向东逐渐转变为两个向南倒转的次级背斜,总体上为向南倒转的复式背斜的核部,其产状及其面理构造与区域构造线完全一致。
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The magmatic sequence includes, from older to younger, early-stage granite and monzonite , tonalite (with preserved amphibolite enclaves), trondhjemite, basic dyke swarm and quartz monzonite sills.
目前除斜长角闪岩包体和基性岩墙群尚未获得同位素年龄外,其他各期侵入体均已获得单颗粒锆石U-Pb测年数据。
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SHRIMP zircon dating suggests that Yajiangqiao trondhjemite was emplaced in 778 ± 11 Ma.
雅江桥奥长花岗岩的SHRIMP锆石U-Pb年龄测定结果为778±11 Ma 。
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Recognition orA-type granite and I-type trondhjemite from available published results.
对区内花岗岩数据重新整理后,区分出碱性A型花岗岩和I型奥长花岗岩。
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I-type granite occurs on north of HongliugouLapeiquan Fault, its chemical composition is similar to that of trondhjemite arisen by Barker (1979), maybe also a product of subduction and collision of oceanic basin in early Paleozoic.
根据SiO〓-Al〓O〓和SiO〓-FeO〓/图解判别显示造山后花岗岩的特征;后者分布在红柳沟—拉配泉断裂以北,其成分与巴克尔1979年提出的奥长花岗岩的成分非常相似,也可能是区内早古生代洋盆俯冲碰撞的产物。
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- 更多网络解释与trondhjemite相关的网络解释 [注:此内容来源于网络,仅供参考]
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trondhjemite aplite:奥长花岗细晶岩
奥长花岗伟晶岩 trondhjemite pegmatite | 奥长花岗细晶岩 trondhjemite aplite | 奥长环斑花岗岩 rapakivi granite
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trondhjemite aplite:奥长花冈细晶岩
"trondhjemite; trondjemite","奥长花冈岩" | "trondhjemite aplite","奥长花冈细晶岩" | "trondhjemite pegmatite","奥长花冈伟晶岩岩"
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trondhjemite porphyrite:奥长花岗璃岩
奥长刚玉岩 plumasite | 奥长花岗璃岩 trondhjemite porphyrite | 奥长花岗伟晶岩 trondhjemite pegmatite
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trondhjemite porphyrite:奥长闪长花冈玢岩
奥长闪长花冈伟晶岩 trondhjemite pegmatite | 奥长闪长花冈玢岩 trondhjemite porphyrite | 浅色奥长花冈岩,奥长闪长岩 trondjemite
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trondhjemite:奥长花岗岩
trona 天然碱 | trondhjemite 奥长花岗岩 | troostite 锰硅锌矿
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