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81.
THE EVOLUTIONARY HISTORY OF THE WEST KUNLUN MOUNTAINS: A TECTONIC RECONSTRUCTION BASED ON STUDIES OF MAGMATISM 相似文献
82.
83.
S. Ferraz-Mello 《Celestial Mechanics and Dynamical Astronomy》1996,65(4):421-437
In the case of the 2:1 and 3:2 resonances with Jupiter, it has not been yet possible to have a complete identification of all chaotic diffusion processes at work, mainly because the time scale of some of them are of an order still out of the reach of precise integrations. A planar Hadjidemetriou's mapping, using expansions valid for high eccentricities and scaled in order to accelerate the diffusion processes, was derived. The solutions obtained with the mapping show huge eccentricity variations in all orbits starting in the middle of the 2:I resonance, when the main short-period perturbations of Jupiter's orbit are considered. The solutions starting in the middle of the 3:2 resonance do not show any important diffusion. 相似文献
84.
大别山超高压变质带中牛凸岭地区低温-高压榴辉岩的发现及其意义 总被引:1,自引:1,他引:0
依据时南大别超高压带腹地的榴辉岩野外地质调查、岩相学和热力学的研究表明,南大别腹地--牛凸岭地区榴辉岩属于低温高压榴辉岩,并未经历超高压变质作用.该地区榴辉岩的共生围岩主要为片岩、片麻岩和斜长角闪岩,石榴石多为自形-半自形,内含大量的早期矿物包体,峰期变质温压条件分别为:T=360~520℃;P=1.3~2.4GPa.对比南大别超高压榴辉岩形成的变质条件,两者压力差可达0.7GPa,约20km厚的地壳深度缺失.结合构造分析牛凸岭单元更类似于桐城-源潭铺高压块体,推测其属于构造上层部位岩片. 相似文献
85.
The ENE-plunging macroscopic folds, traced by calc gneiss interbanded with marble and sillimanite schist within the Peninsular
Gneiss around Suganapuram in the ‘Palghat gap’ in southern India, represent structures of the second generation (D2). They have folded the axial planes of a set of D1 isoclinal folds on stratification coaxially, so that the mesoscopic D1 folds range from reclined in the hinge zones, through inclined to upright in the limb zones of the D2 folds. Orthogonal relation between stratification and axial planar cleavage, and ‘M’ shaped folds on layering locate the
hinge zones of the D1 folds, whereas folds on axial planar cleavage with ‘M’ shaped folds are the sites of the D2 fold hinges. Extreme variation in the shapes of the isoclinal D1 folds from class 1B through class 1C to nearly class 2 of Ramsay is a consequence of buckling followed by flattening on layers
of widely varying viscosity contrast.
The large ENE-trending structures in this supracrustal belt within the Peninsular Gneiss in the ‘Palghat gap’ could not have
evolved by reorientation of NS-trending structures of the Dharwar tectonic province to the north by movement along the Moyar-Bhavani
shear zone which marks the boundary between the two provinces. This is because the Moyar and Bhavani faults are steep dipping
reverse faults with dominant dip-slip component.
Deceased 相似文献
86.
F. R. Cinti L. Cucci D. Pantosti G. D'Addezio M. Meghraoui 《Geophysical Journal International》1997,130(3):595-605
Large historical earthquakes in Italy define a prominent gap in the Pollino region of the southern Apennines. Geomorphic and palaeoseismological investigations in this region show that the Castrovillari fault (CF) is a major seismogenic source that could potentially fill the southern part of this gap. The surface expression of the CF is a complex, 10–13 km long set of prominent scarps. Trenches across one scarp indicate that at least four surface-faulting earthquakes have occurred along the CF since Late Pleistocene time, each producing at least 1 m of vertical displacement. The length of the fault and the slip per event suggest M =6.5-7.0 for the palaeoearthquakes. Preliminary radiocarbon dating coupled with historical considerations imply that the most recent of these earthquakes occurred between 380 BC and 1200 AD, and probably soon after 760 AD; no evidence for this event has been found in the historical record. We estimate a minimum recurrence interval of 1170 years and a vertical slip rate of 0.2-0.5 mm yr-1 for the CF, which indicates that the seismic behaviour of this fault is comparable to other major seismogenic faults of the central-southern Apennines. The lack of mention or the mislocation of the most recent event in the historical seismic memory of the Pollino region clearly shows that even in Italy, which has one of the longest historical records of seismicity, a seismic hazard assessment based solely on the historical record may not be completely reliable, and shows that geological investigations are critical for filling possible information gaps. 相似文献
87.
鲁宗良 《地震地磁观测与研究》1992,13(1):40-45
本文讨论了當熟—太仓5.1级地震前,邻近地区曾多次出现小震震群,形成一个空区之后,在黄海“老震区”出现相对的波形异常。研究结果表明,这些空区和波形异常的出现,除了与地质条件有关外,还显示了出现主震前兆异常的可能性。 相似文献
88.
澜沧—耿马地震前的地震活动条带与空区 总被引:1,自引:0,他引:1
1988年11月6日滇西南发生了澜沧7.6级、耿马7.2级强烈地震,两震相距70公里。本文分析了大震活动的条带与空区特征。这两次地震之前既有M≥4.5地震活动条带,又有M≥3.5地震空区,条带与空区相连接。空区是震前三年多开始出现,震前半年消失的;条带是前一年多时间内形成的,条带的迅速形成深入到空区之内,促使了空区的消失。澜沧7.6级地震发生在两个条带的交汇部位,也是条带的端部、空区的边缘;耿马7.2级地震则发生在空区之内。 相似文献
89.
本文通过历史地震及现今地震活动性的分析、活断层分段理论及地震空区理论的应用、地震平均复发间隔及复发条件概率的估算以及多学科专家综合评估方法的引入,对川西鲜水河-安宁河-则木河断裂和滇东小江断裂带(中-北段)上15个不同段落的地震潜势进行了深入的研究。进一步修正并重新圈绘出位于鲜水河-安宁河-则木河断裂带上的四川省地震重点监视防御区,其范围:北起道孚县的葛卡或者松林口一带,南至西昌市,沿鲜水河-安宁河-则木河主干断裂带展布,全长约350千米。按对未来地震震级估计的不同,该区可分成3段。第1段位于葛卡或松林口至康定之间,震级估计为7±1/4级;第2段位于康定与石棉之间,估计的震级是61/2±1/4;第3段位于石棉至西昌之间,震级估计为7-71/2。此外,研究结果还显示了小江断裂带上的新塘湾和寻甸一嵩明两个段落未来15年内强震发生的概率相对较高。 相似文献
90.
1990年6月14日苏联斋桑7.3级强震发生在重力异常梯度带的拐弯处;强震前存在明显的M_s≥3.5级地震围成的空区;空区走向为北西西向,与斋桑强震发震构造走向一致,长轴约170km。1990年2月14日4.0级地震可视为信号震。最后初步讨论了阿勒泰活动区的地震趋势。 相似文献