Topographic的問題，透過圖書和論文來找解法和答案更準確安心。 我們找到下列地圖、推薦、景點和餐廳等資訊懶人包

Sarrafian’s Anatomy of the Foot and Ankle: Descriptive, Topographic, Functional

為了解決Topographic的問題，作者 這樣論述：

The most comprehensive reference available in this complex area, Sarrafian’s Anatomy of the Foot and Ankle, Fourth Edition, remains the anatomy reference of choice for foot and ankle orthopaedic surgeons and podiatrists. Edited by Drs. Armen S. Kelikian and Shahan K. Sarrafian and featuring original

anatomical dissection photographs prepared by Armen Sarrafian, this classic text has been completely updated throughout, including newly restored dissection photographs. Captures all of today’s clinical knowledge on the anatomy of the foot and ankle, including detailed coverage of functional anatom

y, applied anatomy biomechanics, and cross-sectional anatomy.Contains a new chapter on neurologic motor control of gait and its impact on the foot and ankle, as well as chapters on imaging of the foot and ankle portraying normal anatomy and variants.Features more full-color photographs, new plain fi

lm and magnetic resonance images, and redrawn illustrations to accompany classic dissection photographs.Enrich Your eBook Reading ExperienceRead directly on your preferred device(s), such as computer, tablet, or smartphone.Easily convert to audiobook, powering your content with natural language text

-to-speech.

Topographic進入發燒排行的影片

麗紋石龍子（Plestiodon elegans）在臺灣的族群遺傳分化與隱蔽種

為了解決Topographic的問題，作者林雨昕 這樣論述：

廣泛分布的物種在現今空間上的遺傳結構分布，往往是由過去的地質事件或氣候事件所造成。受惠於分子技術的進步，某些在遺傳上有分化，但在形態上卻非常相似的隱藏譜系得以被發現，顯示兩棲爬行動物在台灣的物種多樣性是被低估的。隱蔽種的發現對於演化理論 、生物地理和保育政策的制定有著深遠 的影響，也能進而探究其種化機制或是種化歷史。麗紋石龍子（ Plestiodon elegans）廣泛分布於中國大陸 、 釣魚台列嶼 、 澎湖以及台灣本島， 是台灣唯一分布海拔跨越 0到 3000公尺左右的蜥蜴，然而對此物種的族群遺傳結構研究甚少。為了 瞭解麗紋石龍子在台灣的遺傳分化，我們在全島 包含 1700公尺以上高海拔

地區 、 澎湖和龜山島，以及代表中國族群的馬祖進行採集， 利用定序取得遺傳資料，包括粒線體的cytochrome b和 ND1以及核基因的 RAG-1和 PRLR片段，重建親緣關係，比較各地族群的遺傳差異和分化時間，並進行形態分析。分子遺傳結果顯示在粒線體片段中，台灣東西部的麗紋石龍子並不呈現單系群。台東附近由低到高海拔的族群為一獨立的單系群，且與台灣其餘族群的遺傳距離高於其他在琉球群島的幾個近緣種。而核基因由於序列相對保守，較無可供辨識的序列特徵 。形態分析結果顯示，台東族群的頭部鱗片 包括眶前鱗、眶後鱗、上睫鱗、下唇鱗、頸鱗）、前肢第二指指墊數和後肢第二、第四趾趾墊數 (RFII、RTII

、 RTIV)、吻肛長（ SVL）以及 頭深 （HD）皆顯著不同於台灣其餘族群。綜合以上，麗紋石龍子在台東的族群應為一獨立的新種，其分類地位必須進行重新的描述。

3D Digital Geological Models: From Terrestrial Outcrops to Planetary Surfaces

為了解決Topographic的問題，作者 這樣論述：

3D DIGITAL GEOLOGICAL MODELSDiscover the practical aspects of modeling techniques and their applicability on both terrestrial and extraterrestrial structuresA wide overlap exists in the methodologies used by geoscientists working on the Earth and those focused on other planetary bodies in the Sol

ar System. Over the course of a series of sessions at the General Assemblies of the European Geosciences Union in Vienna, the intersection found in 3D characterization and modeling of geological and geomorphological structures for all terrestrial bodies in our solar system revealed that there are si

milar datasets and common techniques for the study of all planets--Earth and beyond--from a geological point-of-view. By looking at Digital Outcrop Models (DOMs), Digital Elevation Models (DEMs), or Shape Models (SM), researchers may achieve digital representations of outcrops, topographic surfaces,

or entire small bodies of the Solar System, like asteroids or comet nuclei. 3D Digital Geological Models: From Terrestrial Outcrops to Planetary Surfaces has two central objectives, to highlight the similarities that geological disciplines have in common when applied to entities in the Solar System

, and to encourage interdisciplinary communication and collaboration between different scientific communities. The book particularly focuses on analytical techniques on DOMs, DEMs and SMs that allow for quantitative characterization of outcrops and geomorphological features. It also highlights innov

ative 3D interpretation and modeling strategies that allow scientists to gain new and more advanced quantitative results on terrestrial and extraterrestrial structures. 3D Digital Geological Models: From Terrestrial Outcrops to Planetary Surfaces readers will also find: The first volume dedicated to

this subject matter that successfully integrates methodology and applications A series of methodological chapters that provide instruction on best practices involving DOMs, DEMs, and SMsA wide range of case studies, including small- to large-scale projects on Earth, Mars, the 67P/Churyumov-Gerasime

nko comet, and the MoonExamples of how data collected at surface can help reconstruct 3D subsurface models3D Digital Geological Models: From Terrestrial Outcrops to Planetary Surfaces is a useful reference for academic researchers in earth science, structural geology, geophysics, petroleum geology,

remote sensing, geostatistics, and planetary scientists, and graduate students studying in these fields. It will also be of interest for professionals from industry, particularly those in the mining and hydrocarbon fields.

利用溶液退火自組裝聚苯乙烯-聚二甲基矽氧烷薄膜建構三維奈米圖案成型技術

為了解決Topographic的問題，作者張嫣琳 這樣論述：

摘要三維奈米圖案 (3D Nanopatterning) 的製程中廣泛運用嵌段共聚物自組裝形成多層特徵的微結構已成為微機電系統的主流趨勢。此研究提出了一種有效且簡便的方法，用於開發三維奈米圖案化的新平臺技術。主要策略是使用含高Flory-Huggins Interaction Parameter (χ) 和擁有層板結構的聚苯乙烯-嵌段-聚二甲基矽氧烷 (PS-b-PDMS) 透過溶劑退火的方式來進行順序自組裝。 透過使用PS選擇性溶劑，加上相對溶劑蒸氣壓的調節，可以誘導嵌段共聚物薄膜的自組裝，從而產生各種有序的奈米結構。有趣的是，獨特且單層的六邊形穿孔層板結構 (HPL) 可在薄膜表層對稱的

條件下形成。在反應離子蝕刻後，可以提供具有六邊形孔陣列的二氧化矽單塊。隨後，隨著相對溶劑蒸氣壓的增加，平行圓柱結構的單層可形成並排列在以上六邊形孔陣列的二氧化矽單塊上。在第二次的反應離子蝕刻後，形成線對孔的雙層結構。此外，隨著第二層薄膜厚度的減小，可以在具有平行圓柱陣列的單層薄膜上創建雙層的平行圓柱的正交奈米網格。此外，通過使用強 PS 選擇性溶劑進行退火，可以形成具有六邊形堆積球體的單層，並也可排列在以上六邊形孔陣列的二氧化矽單塊，形成點在孔的雙層結構。透過不同奈米微結構層的疊合，此方法成功創建了一種製造三維納米圖案的新平臺技術，適用於微機電系統應用中。