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1.
The equivalent width calculations for the fundamental vibration rotation band lines of HeH+ have been carried out for a non-DA white dwarf model with an effective temperature of 12 000 K. BothP andR branch lines with rotational quantum numbersJ=3 to 18 were included in the calculations. A search for these lines in helium rich white dwarfs is suggested. 相似文献
2.
Prakash C. Sinha Indu Jain Neetu Bhardwaj Ambarukhana D. Rao Shishir K. Dube 《Natural Hazards》2008,45(3):413-427
The Orissa coast of India is one of the most vulnerable regions of extreme sea levels associated with severe tropical cyclones.
There was extensive loss of life and property due to the October 1999 super cyclone, which devastated large part of the Orissa
coast. The shallow nature of the head bay, presence of a large number of deltas formed by major rivers of Orissa such as Mahanadi
and Dhamra, and high tidal range are responsible for storm surge flooding in the region. Specifically, rising and falling
tidal phases influence the height, duration, and arrival time of peak surge along the coast. The objective of the present
study is to evaluate the tide-surge interaction during the 1999 Orissa cyclone by using nonlinear vertically integrated numerical
models. The pure tidal solution for the head bay region of the Bay of Bengal provides the initial condition for the fine resolution
nested grid Orissa model. However, the feedback from the Orissa model does not affect the head bay model as the study provides
a one-way interaction. Numerical experiments are performed to study the tide-surge interaction by considering various relative
phases of the tidal waves with the surge-wave produced by 1999 Orissa cyclone. The comparison, although utilizing only the
limited estimates of tidal data, appears adequate to assert that the principal features are reproduced correctly. 相似文献
3.
4.
V. P. Gaur Hemraj Survanshi S. K. Shrivastava K. V. Nambiar 《Journal of the Geological Society of India》2016,88(5):603-608
A circular structure, termed as cauldron of volcanic origin, was located near Mohar village in Shivpuri district (M.P.) in the year 2000. Subsequently, the same structure was called as Dhala structure of impact origin. There may be debate over the origin and evolution of this circular structure, but it is characterized by a unique lithological set-up within the Bundelkhand craton. The circular structure is defined by annular disposition of igneous and sedimentary rocks. This includes a set of felsic volcanic rocks and associated breccias named as Mohar Formation, exposed in the outer rim of the circular structure. The inner part of the circular structure has sedimentary sequence, termed as Dhala Formation.The field relations indicate that the Mohar and Dhala foarmations are younger than Bundelkhand granitoid complex but older than Kaimur Group. This period in Indian stratigraphy corresponds to Semri Group which consists of Porcellanite Formation, the rocks of which have formed due to deposition of volcanic ash.The geochronological data and field relations between different litho-units indicate that the Mohar volcanism which generated large volume of volcanic ash was a possible source for the formation of Porcellanite Formation. The deposition of sedimentary sequence in main Vindhyan basin was continued, whereas the volcanic activity in Mohar area continued till H ≈ 1.0 Ga. Since, acid volcanic activity has been reported in different parts of the world at H ≈ 1.0 Ga., it is possible that the Mohar acid volcanic activity is not an isolated event; instead it may be a part of global volcanic activities around H ≈ 1.0 Ga. 相似文献
5.
Nagpal Anushree Hassan Mohammad Siddiqui Masood Ahsan Tajdar Atiqua Hashim Mohammad Singh Abhra Gaur Suman 《GeoJournal》2021,86(2):649-661
GeoJournal - Sanitation is a multidimensional concept alluding primarily to provision of services for safe disposal of human excreta, provision of clean potable water as well as maintenance of... 相似文献
6.
Anticipating the scale invariance of rock fracturing processes, we applied Keilis-Borok’s algorithm M8, originally designed
for identifying times of increased probability (TIPS) of occurrence of strong earthquakes (M < 8.0), retrospectively to Koyna
earthquakes which occurred in the region after the impoundment of the Shivaji Sagar reservoir in 1962. The algorithm which
enables diagnosis of TIPS from the 7th year onwards after the commencement of the earliest available data set showed that
the 5.3 magnitude earthquake of 20 September 1980 indeed occurred within a time of increased probability. This result, apart
from its potential application to recognizing future TIPS in the region, points to selfsimilarity between the premonitory
patterns of natural and induced earthquakes and to scale-invariant nature of their processes. Further, a typical precursory
rise in seismicity followed by a relative quiescence was also found to precede all the three larger earthquakes of the sequence. 相似文献
7.
This paper considers the question of how sensitive inertially guided systems are to variations in the gravity field. There
are systems which use other kinds of information for guidance, such as terrain. But, they will not be considered here. 相似文献
8.
Very little work has been done in generating alternatives to the Poisson process model. The work reported here deals with
alternatives to the Poisson process model for the earthquakes and checks them using empirical data and the statistical hypothesis
testing apparatus. The strategy used here for generating hypotheses is to compound the Poisson process. The parameter of the
Poisson process is replaced by a random variable having prescribed density function. The density functions used are gamma,
chi and extended (gamma/chi). The original distribution is then averaged out with respect to these density functions. For
the compound Poisson processes the waiting time distributions for the future events are derived. As the parameters for the
various statistical models for earthquake occurrences are not known, the problem is basically of composite hypothesis testing.
One way of designing a test is to estimate these parameters and use them as true values. Momentmatching is used here to estimate
the parameters. The results of hypothesis testing using data from Hindukush and North East India are presented. 相似文献
9.
V K Gaur 《Journal of Earth System Science》1981,90(2):147-153
The paper presents values of partial geoidal parametersN, ξ and η which define the departure of the geoid from the reference spheroid, at 1° intervals over the Indian subcontinent. These values represent contributions arising from the gravity anomaly data over the entire earth's surface, except for that from a 6°×6° element around the immediate neighbourhood of the point. Complete values of these parameters at a point can be obtained simply by adding to these partial values, contributions from the 6°×6° element circumscribing that point. The objective of the study was to provide a ready basis for updating the geoidal parameters at the initial reference point as and when the density and quality of local gravity data around it improve. These computations once made, would also facilitate calculation of geoidal parameters at a fairly large number of astro-geodetic stations apart from that at the initial reference point, which should lead to considerably more precise value of the absolute datum of the Indian geodetic dasystem. 相似文献
10.