Seven molybdenite samples from greisen ore body and quartz vein tungsten ore body associated with black tungsten ore were chosen for Re-Os isotopic dating and model age of (141.4±2.2) Ma~(158.2±2.2) Ma were obtained. The isochrone age of molybdenites from greisen type tungsten-tin ore body is (156.8±3.9) Ma, which indicates that its mineralogenetic epoch is at the Middle Jurassic, corresponds to the second stage of early Yanshanian period. And the model age for the samples from greisen ore body and from quartz vein ore body are (150.7±2.4) Ma~(158.2±2.2) Ma and (141.4±2.2) Ma~(151.0±2.4) Ma respectively, which indicates that the mineralization time of the quartz vein ore body is slightly earlier than that of greisen ore body.

文章選取云英巖型礦體及上部石英脈型鎢礦體中與黑鎢礦共生的輝鉬礦7件东南亚黄色毛视频，進(jìn)行Re-Os等時(shí)線年齡測(cè)定800AV久久久凹凸精品，得到其模式年齡為(141.4±2.2) Ma~(158.2±2.2)Ma，其中云英型鎢錫礦體中輝鉬礦等時(shí)線年齡為(156.8±3.9)Ma人人超碰人人爽人人添，成礦時(shí)代為中侏羅世免费看乱伦毛片，對(duì)應(yīng)于燕山早期第二階段；從云英巖礦體中樣品模式年齡為(150.7±2.4)Ma~(158.2±2.2)Ma毛片网毛片官方网，石英脈型礦體中樣品模式年齡為(141.4±2.2)Ma~(151.0±2.4)Ma黄片免费视频高清在线观看。

Apart from the amphibolite enclaves and dyke swarms, the isotopic ages of the magmatic intrusions have been measured. The magmatic sequence and geochronologic framework are as follows: Quartz monzonite, 1825 ± 23 Ma, TDM = 2920Ma; Throndhjemite, 2374 ± 10 Ma, TDM = 3460 Ma; Tonalite, 2604±102 Ma, TDM = 3063 Ma; Monzonite, 3096±17 Ma, TDM = 2978 Ma; Granite, 3605±43 Ma, TDM = 3528 Ma.

在野外建立熱事件相對(duì)序列的基礎(chǔ)上，通過(guò)單顆粒鋯石U-Pb法測(cè)年和Sm-Nd同位素示蹤研究国产在线精品国自产拍影院同，初步建立了該區(qū)早前寒武紀(jì)巖漿活動(dòng)的年代格架：石英二長(zhǎng)巖：1825±23 Ma日韩美乳无码观看网站免费，TDM=2920 Ma欧美性爱与欧美性爱；奧長(zhǎng)花崗巖：2374±10 Ma，TDM=3460 Ma黄色网站一级中文；英云閃長(zhǎng)巖：2604±102 Ma欧美老妇乱惀，TDM=3063 Ma；二長(zhǎng)花崗巖：3096±17 Ma欧美一区888视频在线观看，TDM=2978 Ma国际一级黄色片；花崗巖：3605±43 Ma，TDM=3528 Ma×××www视频。

The research leads to following conclusions: A The age of the ferromanganese contacting with the upper phosphate layer is 14.9 Ma; B The crust had been grown continually without sedimentation interruption since 14.9 Ma, suggesting that it can be used to rebuild the environment of palaeo-ocean and palaeo-climate from 14.9 Ma to 0 Ma; C The sedimentation interruption between the ferromanganese and the upper phosphate layer lasted around 4 Ma; D Between 19 Ma and 22.7 Ma, great phosphatization event happened in this area, which might cause the sedimentation interruption from 22.7 Ma to 14.9 Ma; E The ferromanganese crust began to grow from 75 Ma.

對(duì)超微量Sr同位素測(cè)試得到的富鈷結(jié)殼磷酸鹽年齡進(jìn)行分析認(rèn)為：(1)上部富鈷結(jié)殼與上層白色磷酸鹽化層接觸部位的年齡為14.9 Ma国产精品日韩综合无码专区；(2)自14.9 Ma以來(lái)，結(jié)殼的生長(zhǎng)是連續(xù)的嘿咻国产二区，沉積間斷發(fā)生的可能性非常小免费观看国产又粗又大又爽视频，該樣品可以用來(lái)進(jìn)行14.9 Ma年以來(lái)古海洋、全球變化的重建工作国产在线日韩一区；(3)上層白色磷酸鹽化層與其上部的富鈷結(jié)殼之間存在4 Ma的沉積間斷巨乳爆乳在线；(4)19 Ma~22.7 Ma左右在該區(qū)發(fā)生過(guò)大規(guī)模的磷酸鹽化作用，磷酸鹽化作用可能造成磷酸鹽化時(shí)期(19 Ma~22.7 Ma)和之后4 Ma(19 Ma~14.9 Ma)富鈷結(jié)殼的沉積間斷大乳喷奶水www；(5)結(jié)殼的初始生長(zhǎng)年齡在75 Ma左右爽爽网；(6)老結(jié)殼的生長(zhǎng)速度要遠(yuǎn)低于新結(jié)殼的生長(zhǎng)速度。

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