This age may be the lower limit of the gold ore formation, which means the mineralization time is not earlier than Indo-chinese epoch.

該年齡限定了金礦化年齡的下限，即金礦化不可能早于印支期欧美性高潮视频，但并不能確定金礦化的精確年齡中文一日韩一视频一国产。

Zhongdian is enriched with indo-Chinese epoch neutral acid porphyry as well as one of the porphyry copper deposits in china that was an important breakthrough in the past few years.

中甸地區(qū)是印支期中酸性斑巖集中分布區(qū)，也是我國近年來尋找斑巖銅礦取得重大突破的礦集區(qū)之一2020国内揄拍国内精品。

According to stratum and tectonic characters, judging from the time of tectonic movement and anamorphic characters, the fold in the area happened mainly in Indo-Chinese epoch.

根據地層與構造特征www久草，從構造運動影響的時序及變形特點上判斷，本區(qū)主要在印支晚期才發(fā)生褶皺欧美日韩在线视频黄色。

Meanwhile, the relict stratum of Jurassic in Shanxi and Henan Province can compare with the stratum in Ordos. So we can inferred from that the eastern boundary of the basin is on the east of Luliang Mountain. However, Taihang Mountain has already risen in Indo-Chinese epoch,so the farthest place of the east boundary can only be Taihang Mountain.

同時免费一级在线，山西和河南等地的侏羅系殘留地層與鄂爾多斯可以進行對比，可以推斷99精品一区，盆地的東界在呂梁山以東人成国产免费网站，而太行山在印支期已經隆起，所以盆地的東界最遠只能達太行山九一国产短视频精品一区。

In Jurassic, the western, eastern and northern boundary of the basin had changed in varying degrees, except the south- Qinling orogenic belt rising in Indo-Chinese epoch, which is an always limited boundary. The western of the basin is limited by west-edge thrust nappe belt which formed in early and mid Jurassic.

侏羅紀時6080午夜福利毛片，除了盆地的南界為印支期隆起的秦嶺造山帶外——該造山帶一直是一個限定性的邊界，其他西部欧美粉嫩泬无套在线观看、東部和北部邊界都有不同程度變化深夜在线。

The limited hydrothermal karst and mixed zone beneath the anticline axis controls the porosity distribution of Ordovician System and it is anticipated that surroundings of the axis of fold formed by compressional reverse orverthrusting during Indo-Chinese epoch and the coordinated area of morphology of anticline in the screen of buried hill and that of top surface morphology is the best position for development of the reservoir.

局限的熱液巖溶和裸露的背斜軸部之下的混合帶對千米橋潛山奧陶系孔隙分布具有重要控制作用，預期在印支期擠壓逆沖作用形成的背斜軸部乐播三级黄三区视频免费，特別是潛山內幕背斜形態(tài)與潛山頂面形態(tài)相互協(xié)調的區(qū)域，應是儲層發(fā)育最好的部位日本三级欧美三级人妇视频。

Based on the analysis of tectonic deformation,extensional unconformity,sedimentary facies and paleogeographical rebuilding of southern Tibet,it is recognized that the extensional movement consists of active extension of Hercynian,Indo-Chinese and Early Yanshan epochs,and passive extension of the Himalayan epoch.

藏南特提斯域內伸展運動和伸展作用非常普遍国家aaaa级黄片，根據構造變形分析和伸展不整合、沉積巖相视色4se、古地理再造及巖相對比方法欧美性爱欧美精品二区，對藏南海西期以來的伸展構造進行了較為系統(tǒng)的厘定色影音，確定了海西期、印支期国产美腿美女被操、早燕山期的主動伸展運動和晚燕山期和喜山期的被動伸展作用国产在线.c，并對這些運動特征進行了探討。

East of the deposit is the famous Lincang-Menghai batholithic granite formed during Varisn to Indo-Chinese epoch which has a north-south direction of strike, west is Lancang grouup metamorphic rock.

礦體產在花崗巖與變質巖的構造破碎接觸帶中爱福利视频广场一区二区，成礦與花崗巖漿活動及大氣降水所形成的流體作用有關亚洲色呦呦在线。

As early as the Pleistocene Epoch, China saw the inhabitation of early human beings.

早在更新世初期，就有人類在我國的土地上生活av高速在线网站。

The future, then, to which the epoch of modern economic growth isleading is one of never ending economic growth, a world in which evergrowing abundance is matched by ever rising aspirations, a world inwhich cultural difference is leveled in the constant race to achievethe goods life of material plenty, it is a world founded on belief inscience and the power of rational inquiry and in the ultimate capacityof humanity to shape its own destiny.

所以在伊斯特林看來色污网站免费在线观看，未來的前景不容樂觀：當今經濟發(fā)展的趨勢告訴我們，未來經濟會不斷發(fā)展免费A片一区二区三区视频、永不停歇国产在线精品永久网址，未來世界會是一個財富不斷增長而欲望節(jié)節(jié)上升的世界；一個為達到富裕不斷角逐而導致文化差異盡失的世界亚洲又黄的A片；一個建立在信仰科學和智力并相信人類有最大的能力塑造自己命運的世界又色又污视频网站。