subvolcanic 中文意思是什麼
subvolcanic
解釋
次火山的-
The ore deposit can be named as subvolcanic hydrothermal garnet - diopside - magnetite deposit
可把此礦床定名為次火山水熱石榴子石透輝石磁鐵礦礦床。 -
Primarily summerization on geological characteristics and new progress in scientific research of these deposits are given in this paper, the author proposes that mineralogenesis of mpcd type gold deposit is closely related to meso - neozoic volcanic - subvolcanic action ( cryptoexplosive breccia ), tectonic movement and maturation of organic material
本人概略介紹了其礦床地質特徵、研究現狀及其新進展，並明確提出了該類型金礦床的成礦與中新生代火山-次火山（隱爆角礫巖）作用、構造運動及有機質的作用息息相關。 -
Based on the derivation of metallogenic matters, mineralization and wallrock conditions, the gold deposits are subdivided into three main types : volcanic thermal type, subvolcanic rock - shallow to ultra - shallow porphyry thermal type, and concealed explosive breccia type of gold deposits
根據其金礦成礦物質來源、成礦作用及產出的圍巖條件可劃分為火山熱液型、次火山淺成斑巖熱液型和隱爆角礫巖型金礦床。 -
The gold deposits, related to volcanic - subvolcanic - porphyry metallogenic series of yanshan epoch in northern jiangxi province, belong to one of the most important gold metallogenic series
摘要燕山期火山次火山淺成斑巖金礦成礦系列構成了贛北地區一個重要的金礦成礦系列。 -
The subvolcanic hydrothermal processes show a series responses of alteration rocks with some regularity of space and time evolutions, the main metallogensis was between the silicate alterations ( high - middle temperature and prssure ) and sulfide alterations ( low temperature and pressure )
次火山水熱活動有一系列不同類型，並具一定空間分佈和時間演化規律的蝕變巖響應，主期成礦作用發生在中高溫壓硅酸鹽蝕變與中低溫壓硫化物蝕變之過渡階段。 -
Mazhuangshan gold deposit is of shallow - seated middle - low temperature subvolcanic hydrothermal origin
馬莊山金礦成因為淺成中低溫次火山熱液礦床。 -
Permian series distributed widely in the baisin. lower permian series was composed of acid, neutral, and basic volcanics, subvolcanic rocks, volcanoclastic rocks and few normal sedimentary rocks. from western to eastern, the volcanics transited from acid volcanics to neutral and basic volcanics
二疊系在盆地內部分佈廣泛，下二疊統卡拉崗組主要發育酸、中、基性火山巖、次火山巖、火山碎屑巖及少量正常碎屑巖，由西向東火山巖由中、酸性向中、基性過渡。 -
Cihai iron ore deposit is a subvolcanic - ore pulp intrusive - hydrothermal scouring replacement deposit, which is occurred in the rift of the southern margin of the eastern tianshan mountains in the lower permian epoch
摘要磁海鐵礦床產于早二疊世東天山南緣裂陷槽大地構造環境中，為次火山礦漿侵入熱液充填交代礦床。
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