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111.
辽西地区中侏罗世海房沟组火山岩地球化学特征及其地质意义 总被引:4,自引:0,他引:4
辽西地区中侏罗世海房沟组火山岩的岩石共生组合为粗安岩粗面岩安山岩英安岩 ,属于高钾钙碱性钙碱性火山岩系 ,全岩Rb_Sr等时线年龄为 177.2± 2 8.0Ma。岩石总体上反映出高Al高Na特点 ,SiO2 ≥ 5 6 .99% ,Al2 O3 ≥ 15 .4 5 % ,Na2 O/K2 O≥ 1.35。稀土元素分馏明显 ,(La/Yb) N≥ 14 .80 ,(Ho/Yb) N≥ 1.15 ,贫Yb、Y(Yb≤ 1.4 2× 10 -6,Y≤ 15 .18× 10 -6) ,基本无Eu负异常 (0 .86~ 1.0 3) ,明显亏损Rb、Nb、Zr、Ti,而Sr、Ba、K及LREE富集 ,Rb/Sr值均小于 0 .1,地球化学特征与埃达克岩十分类似 ,属埃达克质岩。Sr、Pb和Nd同位素资料反映出这套火山岩的源岩较深 ,可能为古老的下地壳中基性变质岩部分熔融产物。研究表明 :海房沟组火山岩形成于板内环境 ,与太平洋板块俯冲没有直接关系 ;辽西地区中生代构造应力场的重大转换、广泛的岩浆活动和大规模断陷盆地群的形成与岩石圈拆沉作用密切相关。海房沟组埃达克质岩的确认对探讨辽西地区火山岩浆起源、壳幔相互作用及大陆动力学背景具有重要意义。 相似文献
112.
辽宁北票发现一新的无尾两栖类 总被引:3,自引:0,他引:3
根据一具保存有皮肤印痕的完整骨骼化石,描述了采自辽宁北票黄半吉沟晚侏罗世—早白垩世义县组下部的一新的无尾两栖类,并确立其为一新属、新种—孟氏大连蟾(Dalianbatrachus mengigen.et.sp.nov.)。该化石以其尾杆骨较长,超过荐前椎的总长度,胫腓骨与股骨等长和跗节长小于胫腓骨长的一半而区别于其它两栖类。 相似文献
113.
西天山艾肯达坂组火山岩系同位素定年及其构造意义 总被引:10,自引:1,他引:10
西天山艾肯达坂地区较好发育了艾肯达坂纽红色陆相火山岩建造.它不整合在下石炭统大哈拉军山组之上,未经变形和变质,属于陆陆碰撞晚期的橄榄安粗岩系,其年龄确定是厘定从碰撞造山向陆内构造演化的关键。因此,通过16件新获得的钾氩年龄测值,确定艾肯达坂组火山岩系形成在260Ma~270Ma之间,属早二叠世,而不是过去认为的石炭纪;西天山的陆陆碰撞应在二叠纪末结束,此后进入陆内造山阶段。 相似文献
114.
通过详细研究百岗组沉积相发育特征,将三角洲进行不同类型划分,认为百色盆地东部坳陷的南北两侧分别发育两套不同的沉积体系。沉积响应完整地记录了构造活动情况,在百岗早中期,盆地南部构造抬升强烈,北部构造相对稳定,三角.洲强烈向北西方向进积:百岗晚期,南部构造活动相对稳定,北部构造发生了强烈抬升。南部三角洲在百岗期表现为“发育-发展-稳定-萎缩”的一个完整的演化旋回特点,而北部扇三角洲则体现为“稳定-进积”的过程。整个盆地构造活动在百岗期表现出了两侧构造运动明显的不同步性。 相似文献
115.
栖霞组沉积地球化学特征及其环境意义 总被引:2,自引:1,他引:2
沉积环境的古氧相特征是沉积环境和古海洋特征恢复的重要内容。岩石地球化学特征是判断其形成环境氧化还原条件的重要手段之一。本文以来宾地区铁桥面为重点.通过对栖霞组灰岩的地球化学分析,结合沉积学、古生态学特征.认为栖霞组沉积于贫氧的沉{只背景.是在海水深度和海域的局限程度等沉积条件发生周期性变化的情况下形成的。古氧相地球化学指标V(V十Ni)、Cc/La、U/Th值都适用于该组以钙质沉积为主的沉积物。黄铁矿矿化程度(DOP值)变。化较大.眨映该区多变的古氧相特征。 相似文献
116.
117.
Roberto Torra 《中国地球化学学报》2004,23(3):220-237
Littoral siliciclastic shallow marine horizontal conformable beds (a heterolithic succession), Middle to Late Miocene, outcropping
in northeastern Argentina (Ituzaingó Formation) and overlying transitional conformable horizontal regolithic mantle-rock bed
derived from them (the Pampean and Post-Pampean Formations), were geochemically analyzed. The focus of this study is placed
on the application of geochemical parameter and signature analyses related with the aforementioned geological units, which
are of subcontinental extension into South America. The encountered results show an outstandingly similar geochemical behaviour
between them. The main conclusion is that regolithic mantle-rock beds were derived from the littoral shallow marine mudstone
(silty-argillaceous) beds. This is in oposition to previous aeolian processes proposed early in the 50’s and later. These
mudstone beds constitute important sections of the littoral shallow marine sequence beds (outcropping HST parasequence). Such
regolitization proposed for the Pampean and Post-Pampean Formations predominantly developed in-situ during the Late Pleistocene
and Holocene. The main erosional and mobilized agents were the surface free water (pluvial, fluvial and laminar water sheets)
and vadose water. So, the wind flows and/or the immense air flow hurricanes are of insignificant sedimentological influence.
Otherwise, there is not a proved appropiate sandy-silty reservoir for a reasonable support of the “aeolian hypothesis”, as
well as clear aeolian structures settled in the regolithic mantle-rock bed. In spite of these lines of equality textural-structural
evidence, the geochemical values for both major elements and trace elements, demonstrate that the Miocene heterolithic marine
succession was the mother rock of the overlying regolithic mantle-rock bed, which was formed as an in-situ mantle-rock bed. 相似文献
118.
Beds comprising debrite sandwiched within co-genetic turbidite: origin and widespread occurrence in distal depositional environments 总被引:11,自引:0,他引:11
Co‐genetic debrite–turbidite beds occur in a variety of modern and ancient turbidite systems. Their basic character is distinctive. An ungraded muddy sandstone interval is encased within mud‐poor graded sandstone, siltstone and mudstone. The muddy sandstone interval preserves evidence of en masse deposition and is thus termed a debrite. The mud‐poor sandstone, siltstone and mudstone show features indicating progressive layer‐by‐layer deposition and are thus called a turbidite. Palaeocurrent indicators, ubiquitous stratigraphic association and the position of hemipelagic intervals demonstrate that debrite and enclosing turbidite originate in the same event. Detailed field observations are presented for co‐genetic debrite–turbidite beds in three widespread sequences of variable age: the Miocene Marnoso Arenacea Formation in the Italian Apennines; the Silurian Aberystwyth Grits in Wales; and Quaternary deposits of the Agadir Basin, offshore Morocco. Deposition of these sequences occurred in similar unchannellized basin‐plain settings. Co‐genetic debrite–turbidite beds were deposited from longitudinally segregated flow events, comprising both debris flow and forerunning turbidity current. It is most likely that the debris flow was generated by relatively shallow (few tens of centimetres) erosion of mud‐rich sea‐floor sediment. Changes in the settling behaviour of sand grains from a muddy fluid as flows decelerated may also have contributed to debrite deposition. The association with distal settings results from the ubiquitous presence of muddy deposits in such locations, which may be eroded and disaggregated to form a cohesive debris flow. Debrite intervals may be extensive (> 26 × 10 km in the Marnoso Arenacea Formation) and are not restricted to basin margins. Such long debris flow run‐out on low‐gradient sea floor (< 0·1°) may simply be due to low yield strength (? 50 Pa) of the debris–water mixture. This study emphasizes that multiple flow types, and transformations between flow types, can occur within the distal parts of submarine flow events. 相似文献
119.
The Calafate Formation crops out in south-western Santa Cruz Province, Argentina, and displays a stacking of asymmetrical coarsening–fining-upward cycles. These cycles are interpreted as the product of short-lived transgressive-regressive events in which the coarsening upward part represents sedimentary aggradation with a stable or decreasing sea level. Sedimentological and palynological analyses indicate nearshore marine conditions. Even though the existence of an estuary or incised valley cannot be determined, this is the most probable palaeogeographic model. Based on dinoflagellate cysts, the base of the section is considered to be not older than Maastrichtian. The presence of the oyster Ambigostrea clarae (Ihering) occurring together with the dinoflagellate cyst species Manumiella druggii (Stover) Bujak and Davies and Eisenackia circumtabulata Drugg in the middle part of the section indicates an age no older than late Maastrichtian. According to sedimentological data, deposits representing the Cretaceous–Palaeogene transition would have been eroded, which is confirmed by the presence of Grapnelispora loncochensis Papú. This megaspore is a consistent component of the Maastrichtian assemblages from Patagonia. 相似文献
120.
北京延庆北部地区后城组火山岩岩石化学特征与成因探讨 总被引:3,自引:0,他引:3
根据TAS图解 ,北京延庆北部地区后城组火山属于玄武粗安岩 流纹岩 (和粗面岩 )的双峰式组合。该套火山岩不属于典型的钾玄岩系列 ,在基性岩和中性岩中总体上以碱性系列和向碱性系列过渡的高钾钙碱性系列、钾玄岩系列为主 ,流纹岩类属于富钾质的拉斑系列。该套火山岩轻稀土元素明显富集。玄武粗安岩类岩石没有负铕异常或负铕异常不明显 ,而流纹岩存在明显的负铕异常。延庆北部地区后城组火山岩形成于燕山运动早期或中期阶段的造山变形事件趋于结束时的后碰撞构造环境中。 相似文献