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The patterns of growth strata indicate that the first row of anticlinal belt was developed...

在构造楔沿侏罗系西山窑组煤层向北扩展过程中,台阶状逆断层的大部分位移量沿构造楔顶部的反冲断层向南消减,另一部分位移量则沿西山窑组煤层向北传递至第二排背斜带,在总位移量保持稳定的前提下,第一排背斜带和第二排背斜带在走向上的此消彼长,反映位移量在南、北两个方向上的转换。

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。

It is in accordance with the southward overthrust nappe acting time of South Tianshan orogenic belt.

前渊带以巨厚的浊积岩为特征,在上石炭统上部-下二叠统隆林阶中部台地相地层之上沉积有浊积岩的地质事实表明,前渊带在隆林晚期至中二叠世栖霞期不断向南迁移,这与南天山造山带当时的向南逆掩推覆活动是一致的。

With the appearance of the Yellow River and disappearance of the Late Pleistocene lake in the source area, the Do Qu, on the southern bank of the Yellow River, strengthened southwardly retrogressive erosion and then cut through the Bayanharshan Mountains.

随着现令黄河的形成和晚更新世湖泊的消失,南岸支流之一的多曲向南溯源侵蚀加强,并穿越巴颜喀拉山,夺取了巴颜喀拉山南侧原属于长江流域的贝敏曲和洛曲,使分水岭向南推进了25km,袭夺的时间为晚更新世末期。

The rock belt are composed of malignite, nepheline gabbro, shonkinite, diopside-sienite, hornblende sienite, amphibole-monzonite,granodiorite-granophyre, kaligranite-porphyry, fraidronite, kersanton, precious garnet, olivine alkali-lamprophyre, alkalic-pyroxenolite, alkalic-basalt, latite and trachyte. And the lithofacies of the potassic rock zone include plutonic intrusion, hypabyssal intrusion and eruption.

本文的研究范围是哀牢山-金沙江钾质碱性岩带,该带位于我国西南三江地区的扬子板块和中缅板块三江褶皱区间的缝合带和多个地体边界带,由喜马拉雅期钾质富碱岩浆岩组成;从北往南由新疆塔什库尔干→沱沱河沿→青海囊谦→西藏江达→云南剑川→下关,向南到金平,中国境内该岩带延长达3700km,且向南延至越南境内,平面上岩带呈反&S&形的线形分布特点。

At the end of Oligocene to Miocene, due to lateral extrusion of material in the collisional belt, west Yunnan and adjacent region between the Red River-Ailao Shan and the Saging faults escaped to SSE.

渐新世末—中新世,高原地区的物质侧向挤出,红河—哀牢山断裂和实皆断裂之间的滇西及邻区向南南东脱逸。

The main rivers are Lechang into the county from the northeast corner, by the flow of Shaoguan Wu Gui Town rivers; originated in the northwest and the Yangshan county border Ah fork top and flows from west to east Nanshui reservoir, through the county, import Beijiang rivers of milk; originated in the north-west county and the junction of Yizhang County, Hunan Province Meng Hang Shi Dong Lu, from northwest to southeast through the Daping, bridges, Bibei, Gui Yang, head into the Wujiang River ; originated in the northern foot of the courtyard of the ant hill rock, from north to south flow through Luoyang, large cloth imported Anglo-German city of Tai Tam River.

主要河流有由乐昌流入县境东北角,经桂头镇流向韶关的武江河;发源于县境西北与阳山交界的丫叉顶,由西向东流入南水水库,穿过县城,汇入北江的乳江河;发源于县境西北面与湖南省宜章县交界的猛坑石东麓,由西北向东南经大坪、大桥、必背、桂头流入武江的杨溪河;发源于天井山北麓的蚁岩,由北向南流经洛阳、大布汇入英德市的大潭河。

In Songliao basin, the stronge tectonic inversion occurred in the Late Mingshui Formation, and during the declining of compressive force from the SSE to the NNW, the reactivation of basement faults formed positive inversion faults; released from thermal fluid diapirs, CO2 was migrated upward and then accumulated in inversion structural belts; as the development of fault-style inversion tectonics in the southern part is better than the northern part, and the western is better than the eastern part, CO2 is richer in the south than in the north, richer in the west than in the east in Songliao basin.

松辽盆地强烈的构造反转发生在明水组末期,挤压应力自南南东向北北西方向衰减的过程中,基底断裂复活形成正反转断层,CO2气从热流底辟体中脱出上运而聚集在反转构造带上,断层式反转构造南部比北部发育,西部比东部发育,因此松辽盆地南部比北部、西部比东部CO2气更富集。

Since mid-Miocene, the sea floor spreading stopped and the southwardsubduction of north-wall blocks in the southern boundary zone ofNansha transcrustal layering-block stopped and turned to north-northwestwards thrust of the south-wall blocks.

此时,南海海底扩张停止,南沙南缘的向南俯冲停止而转为南盘岩块的向北—北西逆冲推覆。

Three deep source anomaly belts are related to South Shetland Islands, the Bransfield Strait and Antarctic Peninsula, the north and south belts are positive and negative one in the middle.

深源异常自北向南以正负相间的三个条带状异常分别对应着南设得兰群岛、布兰斯菲尔德海峡和南极半岛,浅源异常则对应着海峡南北缘的两条断裂。

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