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The present invention provides a reinforced tape including a visually transparent backing layer, a reinforcing scrim preferably of fibers made of visually transparent material along one surface of the backing, and a layer of transparent adhesive covering but not totally wetting the reinforcing scrim so that the scrim is visible along the backing layer before the tape is applied to give a user a visual indication of the strength of the tape.

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Jiangnan is the first sign of the train, the window is rolling hills, mist-filled, green river flows slowly, water through mist, fog close to the River, along River Road, lingering fog, mountains are quiet and far-reaching, the water is clean and elegant, only 1 more along the mountain just far seen the mountains of trees, seems to disappear in a sea-green mist, the hill to the far extension of the water to spread , meeting in concert has a unique music, the air seemed to have music with a rhythm, beat, ups and downs, with a 1 wire 1 strand of water vapor, in the gradually dispersed inside ......

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The change of average size of products along the radius at the exist of reactor has also been calculated. The calculated results indicate that the residence time is longer, the average size of products is larger, but the distribution of size is narrower, tending to self-preserving distribution; when the concentrations of reactants increase, the average size of products becomes larger, but the distribution of size becomes narrower; the gradients of reactants are greater, the average size is larger; the increasing of reacting temperature will cause the size of product to be larger under same residence time. The average size of product at the exist of reactor varies along the radius, has a maxim value.

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When semidiurnal tides move from the open sea to offing, they first get the high tide in the mouth of Samen bay, then bifurcate to two branches, one goes along the northwest direction and the other goes along southwest. And it can be easily found that the moving direction of diurnal tides is obviously different from semidiurnal tides.

半日潮波黄片ftp，由浙江東南外海向近海傳播時(shí)，首先在三門灣灣口附近達(dá)到高潮国产专区第一页，之后又分為南北兩支一级在线亚洲欧美日本，一支向西北傳播，另一支向西南傳播天天日日夜夜综合色播，而全日潮波與半日潮波傳播方向有明顯的不同。

Three optimal structures were gotten in this paper by the model of elastic modulus along the grain, elastic modulus in tangential direction, in-plane shearing modulus and laminate rigid:①0/90/0/90/0/90/0/90/0, the outside four veneer is modified, the along grain MOE and MOR are 8377MPa, 60.9MPa respectively; The across grain MOR is 35.1 MPa, and TS is 17.2%.

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牧羊人為我指出了兩條到達(dá)匯交點(diǎn)方向的路人人干干，一條是沿著山脊，即沿著邊墻――倒塌的長(zhǎng)城走欧美三级片黄片高潮；另一條是下到山谷里亚洲免费黄片视频，沿著溝底的小路走。

15 P.m.-- The sunflower field is stretch to the foot of the hill, the height of hill is about 150 m relative. On the hillside I met a sheepherder, He was also surprise to see me and seemed understand my goal after explanation, he come with me up to the hilltop, I look forward to the North, there were no village but mountains and the Great Wall. This section of Great Wall was built in Ming Dynasty (1368-1644), with watchtowers snaking along the mountain ridges, looks spectacular, the collapsed wall along the ridge of mountains, locals call it: BianQiang.

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Results also reveal that, after the construction of Pu-Dai harbor, oblique waves move along both north and south breakwaters of the harbor, which also make nearshore currents move shoreward along the breakwaters.

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Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

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