1) Middle Indo_chinese epoch
印支中期
2) Indo-Chinese epoch
印支期
1.
Basin evolution and sequence stratigraphic framework of south of China during Hercynian cycle to Indo-Chinese epoch;
海西-印支期中国南方的盆地演化与层序格架
2.
Sedimentary characteristics and provenance analysis of Indo-Chinese epoch in the southwest edge of Ordos Basin;
鄂尔多斯盆地西南缘印支期沉积特征及物源
3.
Influence of Qinling Orogenic Movements in Indo-Chinese Epoch to sedimentary characteristics of Yanchang Formation in Ordos Basin;
印支期秦岭造山活动对鄂尔多斯盆地延长组沉积特征的影响
3) Indosinian
印支期
1.
Important significance of regional tectonic regime to metallogenic capacity of Indosinian and Early Yanshanian granites in southeastern Hunan:A case study of Qianlishan and Wangxianling plutons;
区域构造体制对湘东南印支期与燕山早期花岗岩成矿能力的重要意义——以千里山岩体和王仙岭岩体为例
2.
~(40)Ar/~(39)Ar Isotope Dating on Muscovites from Indosinian Raremetal Depositsin Central Altay, Northwestern China;
新疆阿尔泰印支期伟晶岩的成矿年代学研究
3.
Relationship of petro-geochemical characteristics to metallogenic capacity differences between Indosinian and Early Yanshanian granites in southeastern Hunan;
湘东南印支期与燕山早期花岗岩成矿能力差异与岩石地球化学特征关系探讨
4) End of Triassic
印支末期
5) Late Indosinian
印支晚期
1.
Geochemical characteristics of Wangxianling granitic pluton and its constraints on Late Indosinian tectonic setting of Southeast Hunan;
王仙岭岩体地质地球化学特征及其对湘东南印支晚期构造环境的制约
6) Indosinian period
印支期
1.
Many previous dating ages show that these granites were formed at the Hercynian-Indosinian period.
虽然前人对该岩带的侵入年代进行了许多研究工作 ,认为其为海西—印支期产物 ,但由于以往测年方法和技术的一些局限性 ,对于华南是否存在海西期花岗岩一直存在不同意见。
2.
This discovery has not only filled up the gap in Indosinian magmatic record in Wudang orogen but also provided the direct evidence for studying and determining the heat source of deposits in Indosinian period in Wudang region.
在岩石学研究基础上 ,应用Rb -Sr同位素定年技术 ,获得武当造山带印支期花岗斑岩的成岩年龄为 2 37Ma± 19Ma。
3.
During the Indosinian period, the subduction of oceanic crust and closure of Paleo-Tethys cause extensive volcani.
东昆仑中带印支期浅成 -超浅成岩浆岩由闪长玢岩、角闪安山岩、细粒闪长岩和隐爆角砾岩组成。
补充资料：印支半岛
印支半岛就是中南半岛，印度支那地区。它西临孟加拉湾、安达曼海和马六甲海峡，东、南临南海。包括越南、老挝、柬埔寨、缅甸、泰国、新加坡及马来西亚西部。面积206.5万平方千米，占东南亚面积的46％。海岸线长1.17万千米，多重要港湾。地势北高南低，多山地和高原。北部是古老高大的掸邦高原，海拔1500～2000米。众多山脉自南向北呈扇状延伸，形成掸邦高原及南部山、谷相间分布的地形格局。主要山脉自西向东依次为那加山脉、若开山脉；登劳山脉、他念他翁山脉、比劳克东山；长山山脉。3大山序之间的伊洛瓦底江、萨尔温江、湄南河、湄公河、红河自北向南，汹涌奔腾，源远流长。河流上游多穿行于掸邦高原，深切的河谷将高原分为数块，如伊洛瓦底江与萨尔温江之间的东缅高原，萨尔温江与湄公河间的清迈高原，湄公河与红河之间的老挝高原等。一些河流的中下游河谷平原及各河的河口三角洲为主要农业区和人口集中区。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条